1000 Sentences With "glacier" | Random Sentence Generator

During the tour, visitors get to choose between glacier melt kayaking, glacier lake paddleboarding, ice caving and/or glacier camping.

The top is Denman Glacier, the bottom is Scott Glacier.

The Aletsch Glacier is the largest glacier in the Swiss Alps.

Jakobshavn Glacier in Greenland is flowing faster than any other glacier on Earth.

Each glacier inventory includes the location of the glacier, length, orientation, and elevation.

Ironically, Glacier National Park isn't the easiest place to see an active glacier.

Correction: Glacier National Park is in Montana, not Alaska (home to Glacier Bay National Park).

The Athabasca Glacier in the Canadian Rockies is the most visited glacier in North America.

GERMANY 50 Miles Zurich FRANCE SWITZERLAND Detail below Trift Glacier Saas-Grund ALPS Geneva Taconnaz Glacier Planpincieux Glacier Mont Blanc ITALY Eiger Eigergletscher Switzerland Mönch Alps Jungfraujoch Jungfrau 1 mile GERMANY 50 Miles Eiger Zurich Eigergletscher AUSTRIA FRANCE SWITZERLAND Switzerland Detail, right Trift Glacier Mönch Alps Saas-Grund ALPS Geneva Taconnaz Glacier Jungfraujoch Planpincieux Glacier Mont Blanc ITALY Jungfrau 1 mile By The New York Times The company that manages the railway reacted quickly to this finding, installing a highly sensitive, ground-based radar system to continuously monitor the pace of movement within the glacier.

It's an outlet glacier of the larger Mýrdalsjökull glacier, which covers Iceland's most active volcano, Katla.

NASA reports that the region around the Pine Island Glacier, and the Thwaites Glacier, also known as the doomsday glacier, contain enough "highly vulnerable ice" to raise the ocean by four feet.

The mass balance of glacier surface represents the most direct link between glacier change and climate forcing.

For example, the glaring vanishing act that is the Grinnell Glacier in Glacier National Park can be seen via a "very challenging day hike from the Many Glacier area," according to the park.

Young visitors embark on a guided glacier tour at an exposed portion of the Aletsch Glacier on Aug.

The new Gatorade Zero comes in five fruity flavors: orange, lemon-lime, glacier cherry, glacier freeze and berry.

That makes Glacier Deep Archive an extension to the existing AWS Glacier service, but at a far lower price.

In Sichuan Province, tourists flock to Hailuogou National Glacier Forest Park, and Yunnan Province has the popular Mingyong Glacier.

The glacier, which is described in a paper published yesterday in Geophysical Research Letters, is called Pine Island Glacier.

Glacier scientist Shea suggests seeing Athabasca Glacier, right off of the 114-mile Icefields Parkway in the Canadian Rockies.

And where there's a glacier, there's sometimes a glacier lake to see, which is even more spectacular at sunrise.

The Jakobshavn glacier, also called the Ilulissat glacier, has been called Greenland's "fastest-flowing and fastest-thinning" by NASA.

Huss told the news outlet there are only 26,000 square meters of ice left in the glacier and it will be the first glacier in the country to be taken off the Swiss glacier surveillance network.

The expedition was part of the International Thwaites Glacier Collaboration, a series of research projects aimed at understanding the glacier.

The glacier, once known as Okjökull ("jökull" means glacier in Icelandic) lost its status as a glacier in 2014, since it had shrunk below one square mile and was barely 50 feet deep, according to The Guardian.

"When my family and I have eaten lunch on Grinnell Glacier, the glacier has receded during lunch," he said of Glacier National Park, where the number of ice sheets has dropped to 25 from 150 in 133.

But now, glacier scientists have confirmed that even Taku — a robust glacier 4,860 feet thick — has finally started to lose mass.

"Ok is the first Icelandic glacier to lose its status as a glacier," the plaque presented Sunday reads in English and Icelandic.

Researchers will travel to the world's largest mountain glacier systems, collecting microorganisms from hundreds of glacier-fed streams and analyzing their genomes.

Pine Island Glacier, along with its neighbor Thwaites Glacier, effectively act as arteries connecting the West Antarctic ice sheet to the ocean.

The glacier has contributed more to sea level rise than any other glacier in the Northern Hemisphere, though recently, that has slowed.

More than 500 Swiss glaciers have been lost since 1003, and 2019 saw the Pizol glacier removed from the country's glacier monitoring network.

Ice loss from the two glaciers studied—the Pine Island Glacier and Thwaites Glacier—is already Antarctica's largest contribution to sea level rise.

The Lamplugh Glacier rock avalanche (Image: Paul Swanstrom/Mountain Flying Service)An extraordinarily large landslide has been discovered near Glacier Bay in southeast Alaska.

Undoubtedly, Alaska's receding Mendenhall Glacier is one of the best places to both witness a momentous glacial recession and learn about the diminished glacier.

Climate scientists tend to watch this glacier closely, usually alongside the nearby Pine Island Glacier, which is also flowing rapidly into the Amundsen Sea.

But it was buttressing the Pine Island Glacier, acting as a barrier between the warmer sea water and the ice that makes up the glacier.

One particularly large glacier called Pine Island Glacier made headlines in 2017, when it lost a chunk of ice four times the size of Manhattan.

As reported by The Washington Post, the smoke has been turning normally white glaciers, such as Tasman Glacier and Franz Josef Glacier, a brown color.

Glacier National Park, Through Foreign Eyes My National Park: Glacier National Park An earlier version of this article erroneously included the Columbia River Gorge, Ore.

We were walking in the "ablation zone," the part of the glacier where melting exceeds accumulation; it typically comprises the lower third of a glacier.

Haefeli Glacier, Finsterwalder Glacier, Sharp Glacier, Sölch Glacier, Wilkinson Glacier, Koriten Glacier, Dabrava Glacier, Brückner Glacier and Antevs Glacier feed the fjord.

Glaciers include Baltoro Glacier, Biafo Glacier, Siachen Glacier, Trango Glacier and Godwin-Austen Glacier.

Later inventories of the World Glacier Monitoring Service under the direction of Fritz Müller, who worked on glacier inventories internationally, included the Axel Heiberg Island glacier. Other glaciers and ice caps in the Queen Elizabeth Islands include the Agassiz Ice Cap, Benedict Glacier, Disraeli Glacier, Eugenie Glacier, Gull Glacier, Parrish Glacier, Sven Hedin Glacier and the Turnabout Glacier.

The Park is named for its abundant tidewater and terrestrial glaciers, numbering 1,045 in total. There are seven tidewater glaciers in the park: Margerie Glacier, Grand Pacific Glacier, McBride Glacier, Lamplugh Glacier, Johns Hopkins Glacier, Gilman Glacier, and LaPerouse Glacier. (High tide-water glaciers also include Riggs Glacier, Reid Glacier, Lituya Glacier, and North Crillon Glacier.) Four of these glaciers actively calve icebergs into the bay. In the 1990s, the Muir Glacier receded to the point that it was no longer a tidewater glacier.

San Rafael Glacier, Chile. Perito Moreno Glacier, Argentina as seen from space. Pastoruri Glacier, Peru. Glacier Lagoon, Bolivia.

The near by Glaciers are Ikualari Glacier, Billanlari Glacier, Surajkund Glacier all this glacier joins the main glacier Milam Glacier from there emerges the river Goriganga River that later joins the Kali River at Jauljibi.

Eleven named glaciers descend from Mount Baker. Two additional glaciers (Hadley Glacier and Sholes Glacier) descend from lower slopes detached from the main glacial mass. The Coleman Glacier is the largest; it has a surface area of . The other large glaciers—which have areas greater than —are Roosevelt Glacier, Mazama Glacier, Park Glacier, Boulder Glacier, Easton Glacier, and Deming Glacier.

Vasuki Parbat is surrounded by the Vasuki Glacier on the west side and Sundar Bamak (Glacier) on the east side northern side is surrounded by Chaturangi Glacier. Vasuki Glacier and Sundar Glacier merge with Chaturangi Glacier. Chaturangi Glacier merge with Gangotri Glacier from the snout of Gangotri Glacier emerges Bhagirathi river also called Ganga or Ganges after it meets Alaknanda at Dev Pryag.

Sirmilik Glacier Sirmilik Glacier Sermilik Glacier is a glacier located in the southern Byam Martin Mountains of Bylot Island, Nunavut, Canada.Geonames: Sermilik Glacier It lies in Sirmilik National Park.

Lied Glacier is a glacier close north of Cape Arkona on the southwest side of Heard Island in the southern Indian Ocean. To the southeast of Lied Glacier is Gotley Glacier, whose terminus is located between Cape Arkona and Cape Labuan. Cape Arkona separates Lied Glacier from Gotley Glacier. To the north of Lied Glacier is Abbotsmith Glacier.

Pilz Glacier (also known as Pit Glacier) is in Wenatchee National Forest in the U.S. state of Washington and is on the north slopes Luahna Peak. Pilz Glacier descends from . An arête separates Pilz Glacier from Butterfly Glacier to the west. Pilz Glacier is within the Glacier Peak Wilderness and is just over southeast of Glacier Peak.

Gondogoro Glacier () or Gondoghoro Glacier is glacier near Concordia in Gilgit-Baltistan, Pakistan. It serves as an alternative means to reach Concordia; the confluence of Baltoro Glacier and Godwin-Austen Glacier.

Sitkum Glacier is located on the west slopes of Glacier Peak in the U.S. state of Washington. As is true with all the glaciers found on Glacier Peak, Sitkum Glacier is retreating. Sitkum Glacier is immediately south of Scimitar Glacier.

Peck Glacier is an alpine glacier in Roosevelt National Forest in the U.S. state of Colorado. Peck Glacier is northwest of Fair Glacier.

Weyprecht Glacier () is a glacier in Jan Mayen. It is the longest glacier located in the Beerenberg area.Weyprecht Glacier, Jan Mayen - Geographical Names The glacier is named after Austro-Hungarian Arctic explorer Karl Weyprecht.

It stands between two glacier Bamchu Glacier and Sakram Glacier on the western side. Both the glacier flows down from west to east and joins Milam Glacier. Further down south east from the snout of Milam glacier emerges Goriganga River that later joins the Kali River at Jauljibi. On the western side Uttari Nanda Devi Glacier flows down north and joins Uttari Rishi Glacier from the snout of Uttari Rishi Glacier emerges Rish Ganga.

Gem Glacier is the smallest named glacier in Glacier National Park (U.S.). Located on the east (Glacier County) side of the Continental Divide arête known as the Garden Wall, the glacier is situated on the cliff face above the better known Grinnell Glacier. Gem Glacier is a hanging glacier, and drapes down from the north face of the steep arete to which it is attached. Gem Glacier is only in area and is far below the threshold often cited as qualifying as an active glacier.

The Johan Peninsula is located on the eastern coast of Ellesmere Island, a part of the Qikiqtaaluk Region of the Canadian territory of Nunavut. It stretches eastward into Nares Strait. Buchanan Bay is to the north, Rosse Bay to the east (separating the peninsula from Pim Island), and Baird Inlet lies to the south. There are several glaciers surrounding the peninsula, including Leffert Glacier, Jewell Glacier, Saate Glacier, Fram Glacier, Twin Glacier, Alfred Newton Glacier, MacMillan Glacier, Allen Glacier, Green Glacier, and Small Glacier.

The Arolla Glacier () is a long glacier (2005) situated in the Pennine Alps in the canton of Valais in Switzerland. In 1973 it had an area of . The Glacier d'Arolla is in fact composed of two glacier: the Glacier du Mont Collon and the Haut Glacier d'Arolla.

Mikado Glacier () is a glacier on the north side of Mahler Spur, flowing west- northwest into Sullivan Glacier near the junction with Gilbert Glacier in northern Alexander Island, Antarctica. The glacier was so named by the UK Antarctic Place-Names Committee in 1977 in association with nearby Gilbert Glacier and Sullivan Glacier, after the 1885 operetta The Mikado.

Nama glacier this 5 km long glacier flows NE towards Kuthi. The glacier has three feeder streams. Rama glacier The biggest glacier of this range flows NW from Brammah Parvat and Cheepaydang to the main Darma valley. Lebong glacier This short glacier lies on the W side of the Shin la and terminates at 4400 m above Bidang grazings.

Buxton Glacier is a glacier flowing northeast between Heaney Glacier and Cook Glacier, on the north coast of the island of South Georgia, immediately south of Mount Skittle. The terminus of Buxton Glacier is located at Saint Andrews Bay. Buxton Glacier is close to Ross Glacier, which is leaving a gravel beach in the wake of its retreat.

Chocolate Glacier is located on east slopes of Glacier Peak in the U.S. state of Washington. The glacier descends from to and is partially connected to Cool Glacier which lies to its south just below the summit of Glacier Peak. As is true with all the glaciers found on Glacier Peak, Chocolate Glacier is retreating. Chocolate Glacier retreated approximately between 1906 and 1946, however during a cooler and wetter period from about 1950 to 1979, the glacier advanced .

Cool Glacier is located on east slopes of Glacier Peak in the U.S. state of Washington. The glacier descends from to and is partially connected to Chocolate Glacier which lies to its north just below the summit of Glacier Peak. As is true with all the glaciers found on Glacier Peak, Cool Glacier is retreating. Cool Glacier retreated approximately between 1850 and 1946, however during a cooler and wetter period from about 1950 to 1979, the glacier advanced.

Clarence Island seen from northeast with (left to right) Cape Bowles; Dobrodan Glacier and Highton Glacier surmounted by Urda Ridge; Treskavets Glacier, Orcho Glacier and Banari Glacier surmounted by Ravelin Ridge; and Cape Lloyd Orcho Glacier (, ) is long and wide glacier on the east side of Ravelin Ridge on Clarence Island in the South Shetland Islands, Antarctica situated north of Treskavets Glacier and south-southwest of Banari Glacier. It flows eastwards and enters the Southern Ocean north of Gesha Point. The glacier is named after the Bulgarian rebel leader Orcho Voyvoda (1829-1911).

Map of Sentinel Range. Gerila Glacier (, ) is long and wide glacier on the east side of the main crest of north-central Sentinel Range in Ellsworth Mountains, Antarctica. It is situated north of Burdenis Glacier and south of Fonfon Glacier. The glacier drains the saddle of the twin peak of Long Gables, flows northeastwards and together with Delyo Glacier and Burdenis Glacier joins upper Ellen Glacier north of Bruguière Peak.

Glaciologists researching the North Cascades found that all 47 monitored glaciers are receding while four glaciers—Spider Glacier, Lewis Glacier, Milk Lake Glacier and David Glacier—have disappeared completely since 1985. The White Chuck Glacier (near Glacier Peak) is a particularly dramatic example. The glacier area shrank from in 1958 to by 2002. Between 1850 and 1950, the Boulder Glacier on the southeast flank of Mount Baker retreated .

Rutgers Glacier () is a steep glacier on the west side of the Royal Society Range in the Ross Dependency, Antarctica. Rutgers Glacier descends southwest from Johns Hopkins Ridge and Mount Rucker to enter the Skelton Glacier. Abbott Spur separates the lower ends of Rutgers Glacier from Allison Glacier.

Clark Glacier is in Wenatchee National Forest in the U.S. state of Washington and is on the east slopes of Clark Mountain. Clark Glacier descends from . Clark Glacier is connected to Richardson Glacier to the west at its upper margins. Clark Glacier has also been known as Walrus Glacier.

Satellite image of the Pashleth Glacier The Pashleth Glacier is a glacier south of the Machmell River and west of the Klinaklini Glacier in southwestern British Columbia, Canada.

Clarence Island seen from northeast with (left to right) Cape Bowles; Dobrodan Glacier and Highton Glacier surmounted by Urda Ridge; Treskavets Glacier, Orcho Glacier and Banari Glacier surmounted by Ravelin Ridge; and Cape Lloyd Banari Glacier (, ) is the long and wide glacier on the east side of Ravelin Ridge on Clarence Island in the South Shetland Islands, Antarctica situated north-northeast of Orcho Glacier. It flows northeastwards and enters Smith Cove. The glacier is named after the settlement of Banari in Northern Bulgaria.

The mountain and its climate supports the Matier Glacier, Stonecrop Glacier, and Tszil Glacier on the northern slopes.

Vigne Glacier () is a glacier in Gilgit–Baltistan, Pakistan near Gondogoro Glacier and Baltoro Glacier. The glacier is named after Godfrey Vigne (1801-1863), an early British traveller in Kashmir and Baltistan. It provides access to Gondogoro (La) Pass.

Vasuki Parbat is surrounded by the Vasuki Glacier on the west side and Sundar Bamak (Glacier) on the east side northern side is surrounded by Chaturangi Glacier both east and west merge with Chaturangi Glacier. Chaturangi Glacier merge with Gangotri Glacier from the snout of Gangotri Glacier emerges Bhagirathi river also called Ganga or Ganges after it meets Alaknanda at Devpryag.

The Whitney Glacier is a glacier situated on Mount Shasta, in the U.S. state of California. The Whitney Glacier is the longest glacier and the only valley glacier in California. In area and volume, it ranks second in the state behind the nearby Hotlum Glacier. In 1986, the glacier was measured to be deep and over three km in length.

11-13 Mount Wrangell is almost entirely covered by an icefield that persists from year to year. The largest glacier on Wrangell is Nabesna Glacier, the source of the Nabesna River. Other glaciers on Mount Wrangell include Cheshnina Glacier, Chetaslina Glacier, Chichokna Glacier, Dadina Glacier and Copper Glacier. Wrangell was the first high volcano in the Wrangell range to be climbed.

Vahsel Glacier () is a glacier on the northwestern side of Heard Island in the southern Indian Ocean. It flows west into South West Bay, between Erratic Point and Cape Gazert. Immediately to the north of Vahsel Glacier is Schmidt Glacier, whose terminus is located between Mount Drygalski and North West Cornice. To the south of Vahsel Glacier is Allison Glacier, whose terminus is located south of Cape Gazert, which separates Allison Glacier from Vahsel Glacier.

Kanikula Glacier., also known as Little Tokositna Glacier, is an long glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates in a series of glacial amphitheaters in the south side of the range, moving southeast past Mount Goldie and ending before the valley of Tokositna Glacier. Variant forms and spellings of the name include K'enik'ela Li'a, Kahnicula Glacier, Kanicula Glacier and Little Tokasitna Glacier.

North Guardian Glacier is located on east slopes of Glacier Peak in the U.S. state of Washington. The glacier descends from to and is partially connected to Chocolate Glacier which lies to its south. As is true with all the glaciers found on Glacier Peak, North Guardian Glacier is retreating. North Guardian Glacier retreated approximately between 1850 and 1946, however during a cooler and wetter period from about 1950 to 1979, the glacier advanced modestly.

Lhatu Dhura stands at the head of the western side of Timphu Glacier and between Timphu glacier and Pachhu Glacier. Both the glacier flows down from west to east and the streams emerges from these glacier Timphu Gad and Pachhu Gad joins Goriganga River. Goriganga River emerges from the snout of Milam glacier that later joins the Kali River at Jauljibi. On the western side Uttari Nanda Devi Glacier flows down north and joins Uttari Rishi Glacier from the snout of Uttari Rishi Glacier emerges Rish Ganga.

Red Eagle Glacier is a glacier remnant (glacieret) in Glacier National Park in the U.S. state of Montana. The glacieret is a hanging glacier located to the southeast of Mount Logan and Logan Glacier. Between 1966 and 2005, Red Eagle Glacier lost 53 percent of its surface area and now covers less than which is below the threshold to qualify as an active glacier. Comparing images of the glacier taken in 1914 with those from 2009, indicates that the glacier has experienced extensive retreat.

Clarence Island seen from northeast with (left to right) Cape Bowles; Dobrodan Glacier and Highton Glacier surmounted by Urda Ridge; Treskavets Glacier, Orcho Glacier and Banari Glacier surmounted by Ravelin Ridge; and Cape Lloyd. Treskavets Glacier (, ) is long and wide glacier on the east side of Ravelin Ridge on Clarence Island in the South Shetland Islands, Antarctica situated north of Highton Glacier and south of Orcho Glacier. It drains the slopes of Jerez Peak, flows northeastwards and enters the Southern Ocean south of Gesha Point. The glacier is named after the settlement of Treskavets in Northeastern Bulgaria.

It is surrounded by glaciers on all the sides: Kalindi Glacier on the southern side, Arwa Glacier on the eastern side, Mana Glacier on the northern side and Raktavarn Glacier on the western side. Kalindi Glacier joins with Chaturangi Glacier and Chaturangi Glacier joins with Gangotri Glacier from there emerges the river Bhagirathi the main tributaries of river Ganga. Mana glacier on the other side drains into Jadh Ganga also called Jahanvi Ganga that joins Bhagirathi near Bhaironghati. Arwa nala starts from Arwa glacier that drains into Saraswati river near Ghastoli that ultimately joins Alaknanda river at Mana village.

The Malaspina Glacier is the largest piedmont glacier in North America, Hubbard Glacier is at the longest tidewater glacier in Alaska, and the Nabesna Glacier is the world's longest valley glacier, at more than . Glaciers in Wrangell–St. Elias are mostly in retreat. The Bagley Icefield has grown thinner and its glaciers have retreated, including portions feeding Malaspina Glacier, which is stagnant or retreating.

Location of Pernik Peninsula on Loubet Coast, Antarctic Peninsula. Peyna Glacier (, ) is the 11.4 km long and 3 km wide glacier on Pernik Peninsula, Loubet Coast in Graham Land, Antarctica, situated southwest of Blagun Glacier and northeast of Murphy Glacier. It flows northwestwards along Lane Ridge, and joins Murphy Glacier and Wilkinson Glacier. The glacier is named after the settlement of Peyna in Northern Bulgaria.

Kennedy Glacier is located on northwest slopes of Glacier Peak in the U.S. state of Washington. As is true with all the glaciers found on Glacier Peak, Kennedy Glacier is retreating. During the Little Ice Age, Kennedy Glacier extended down to an altitude of and was connected to Scimitar Glacier to the south. From about 1850 to 1952, the glacier lost of its length.

Kaparoqtalik Glacier in the southern Byam Martin Mountains Tip of the tongue of Kaparoqtalik Glacier Kaparoqtalik Glacier is a glacier located in the southern coast of the Byam Martin Mountains on Bylot Island, Nunavut, Canada.GeoNames: Kaparoqtalik Glacier It lies in Sirmilik National Park.

Sleipner Glacier (), is a glacier in eastern Greenland. This glacier was named after Sleipner, Odin's mythical eight-legged flying horse.

Map of Sentinel Range. Delyo Glacier (, ) is the 8 km long and 2.7 km wide glacier on the east side of the main crest of north-central Sentinel Range in Ellsworth Mountains, Antarctica. It is situated northwest of Rumyana Glacier and south of Burdenis Glacier. The glacier drains the north slopes of Mount Giovinetto and the east slopes of Mount Viets, flows northeastwards and together with Burdenis Glacier and Gerila Glacier joins upper Ellen Glacier north of Bruguière Peak.

Milk Lake Glacier is located in the Glacier Peak Wilderness in the U.S. state of Washington. The glacier is within Mount Baker-Snoqualmie National Forest and a little over northwest of Glacier Peak. Milk Lake Glacier disappeared sometime between 1984 and 1997 and by 2005, Milk Lake was situated where the glacier had once been.

Navajo Glacier is an alpine glacier in Roosevelt National Forest in the U.S. state of Colorado. Navajo Glacier is on the north slope of Navajo Peak and about south of Isabelle Glacier.

Arago Glacier () is a glacier flowing into Andvord Bay just northwest of Moser Glacier, on the west coast of Graham Land.

Blagun Glacier (, ) is the 13 km long and 2.3 km wide glacier on Pernik Peninsula, Loubet Coast in Graham Land, Antarctica, situated southwest of Dolie Glacier and northeast of Peyna Glacier. It flows northwestwards between Lane Ridge and Hodge Ridge, and joins Wilkinson Glacier. The glacier is named after the settlement of Blagun in Southern Bulgaria.

Depot Glacier is in North Cascades National Park in the U.S. state of Washington, on the northeast slopes of Mount Redoubt. Depot Glacier descends from the . Melt from the glacier feeds into Depot Creek which flows into Chilliwack Lake. The Redoubt Glacier lies to the east while the West Depot Glacier is separated from Depot Glacier by a ridge.

Chickamin Glacier is in the U.S. state of Washington. Chickamin Glacier is in Wenatchee National Forest and flows north from Dome Peak and Sinister Peak, descending from nearly . Chickamin Glacier is separated from Dome Glacier to the south and Dana Glacier to the west by arêtes. The relatively narrow tongue of the wide glacier retreated between 1998 and 2006.

The institute has been featured in a book Study Science at the Glacier Institute written by Bruce Larkin.Larkin, Bruce. (2007) Study Science at the Glacier Institute . Glacier Institute has two campuses: its "Glacier Park Field Camp," located inside the West Glacier entrance of Glacier National Park, and its "Big Creek Outdoor Education Center," located in the Flathead National Forest.

Spider Glacier is in Wenatchee National Forest in the U.S. state of Washington and is to the east of Phelps Ridge. Spider Glacier is long but very narrow at only in width. Spider Glacier is southeast of Lyman Glacier. This Spider Glacier is not to be confused with another of the same name nearby, Spider Glacier (Spider Mountain, Washington).

Hinlopenbreen ("Hinlopen glacier") is a glacier stream in Spitsbergen, Svalbard. The glacier debouches into Vaigattbogen in Hinlopen Strait. The glacier has a length of about 70 km, and drains an area of about .

Grant Glacier is located in the US state of Montana in Flathead National Forest. The glacier is situated in a cirque and lies below the east slopes of Mount Grant (). Grant Glacier is southeast of Stanton Glacier and both west of Glacier National Park (U.S.). Images taken of the glacier in 1902 and from the same vantage point in 1998 indicate that the glacier retreated substantially during the 20th Century.

Swiftcurrent Glacier is in Glacier National Park in the U.S. state of Montana.The glacier is on the east (Glacier County) side of the Continental Divide arête known as the Garden Wall. Swiftcurrent Glacier is one of several glaciers that are being monitored to determine stream flow alterations that occur due to glacial retreat. Compared to other glaciers in Glacier National Park, Swiftcurrent Glacier has experienced relatively slow retreat.

Scimitar Glacier is located on the west and northwest slopes of Glacier Peak in the U.S. state of Washington. As is true with all the glaciers found on Glacier Peak, Scimitar Glacier is retreating. During the Little Ice Age Scimitar Glacier was connected to Kennedy Glacier to the north. From about 1850 to 1946, the glacier retreated , but advanced during a colder and wetter period lasting until about 1980.

To the east of Baudissin Glacier is Challenger Glacier, whose terminus is located at the eastern side of Corinthian Bay, close west to Saddle Point. To the south of Baudissin Glacier is Schmidt Glacier, and to the northwest is Atlas Cove. Kildalkey Head is west of Schmidt Glacier. To the south of Schmidt Glacier is Vahsel Glacier, whose terminus is at South West Bay, between Erratic Point and Cape Gazert.

In the case of the most glaciers such as the Taku Glacier the glacier will eventually build a terminus shoal that is above water and calving will essentially cease. This will eliminate this loss of ice from the glacier and the glacier can continue to advance. Taku Glacier and Hubbard Glacier have been in this phase of the cycle. Taku Glacier which has been advancing for 120 years no longer calves.

Neola Glacier or Athasi-Balati Glacier is the Himalayan glacier situated in the eastern part of Uttarakhand in the Pithoragarh district of India. Neola Glacier is located at the base of the five peaks of Panchchuli in the Lassar Yankti valley. The Neola Glacier combines with the Saun Glacier to form the famous Panchchuli Glacier. Sona and Neola glaciers serve as the route to climb the Panchchuli peaks from the east.

Blackfoot Glacier is the second largest of the remaining 25 glaciers in Glacier National Park, Montana. Blackfoot Glacier is just to the north of Blackfoot Mountain and near Jackson Glacier. The glacier was most recently measured in 2005 at , yet when first documented in 1850, the glacier also included the now separate Jackson Glacier and together, they covered . In 1850, there were an estimated 150 glaciers in the park.

The Depot Glacier lies to the west of Redoubt Glacier.

The other two are the Khumbu Glacier and Rongbuk Glacier.

In the 19th century, Tsaneri Glacier was the second largest glacier in Georgia after the glacier Tviberi Glacier: according to topographic maps from 1887, the surface of the glacier with the connected Nageba Glacier was about 48.9 km² Levan G. Tielidze Glacier change over the last century, Caucasus Mountains, Georgia, observed from old topographical maps, Landsat and ASTER satellite imagery The Cryosphere 2016 719-720 . In 1960, the area of Tsaneri Glacier without the Nageba Glacier was about 28.3 km2 . In the following years, the glacier was divided into the southern and northern parts, which in 2014 covered respectively 12.6 km² and 11.5 km².

Map of northern Sentinel Range Sabazios Glacier (, ) is the long and wide glacier on the east side of northern Sentinel Range in Ellsworth Mountains, Antarctica. It is situated south of Newcomer Glacier, west of Anchialus Glacier, north of Embree Glacier, and east of Zhenda Glacier and Skaklya Glacier. The glacier drains the east slopes of Mount Alf and Mount Sharp, and the north slopes of the side ridge that trends 9.15 km from Mount Dalrymple on the main crest of Sentinel Range east-northeast to Robinson Pass, flows northwards and joins Newcomer Glacier northwest of Mount Lanning in Sostra Heights. The glacier is named after the Thracian god Sabazios.

McCall Glacier,Beckey, p. 71. Meade Glacier, and Packwood Glacier,Beckey, p. 334. along with numerous smaller permanent snowfields.Beckey, pp. 70–73.

Glacier Mints resemble miniature blocks of ice and are clear and translucent. Companion products are Fox's Glacier Fruits and Fox's Glacier Dark.

The Gangotri Glacier on the east side and Vasuki Glacier on the west side and Chaturangi Glacier on the north. From the snout of Gangotri Glacier emerges Bhagirathi river also called Ganga or Ganges.

Tungnafellsjökull and the Icelandic flag Tungnafellsjökull (Icelandic for "Tungna-fells glacier" or "tongue-fells glacier") is a glacier and volcano in Iceland. It has an elevation of and is located northwest of Vatnajökull glacier.

Monacobreen as seen from Liefdefjord Monacobreen is a glacier in Haakon VII Land on Spitsbergen, Svalbard. The glacier debouches into Liefdefjorden. Former names of the glacier include Glacier de Monaco and Liefde Bay-bræ.

It is surrounded by glaciers on all the sides: Kalindi Glacier on the southern side, Arwa Glacier on the eastern side, Mana Glacier on the northern side and Raktavarn Glacier on the western side.

Doran Glacier () is a glacier between Sollas Glacier and Marr Glacier on the north slope of the Kukri Hills, Victoria Land. It was named by the Advisory Committee on Antarctic Names in 1997 from association with Doran Stream, which flows north from this glacier into Taylor Valley.

Sven Hedin Glacier is a glacier north of Princess Marie Bay on central Ellesmere Island, Nunavut, Canada. The glacier has the name of Sven Hedin. The Oxford University Ellesmere Land expedition visited the glacier in the year 1935. The Glacier appeared to be advancing in 1935.

It is surrounded by glaciers on both the sides Suralaya Glacier on the western side, sweta Bamak on the eastern side, Both the glacier joins with Chaturangi Glacier and Chaturangi Glacier joins with Gangotri Glacier from there emerges the river Bhagirathi the main tributaries of river Ganga.

Sunset Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates near Scott Peak, moving southwest, then northwest. Sunrise Glacier is nearby.

Romanche Glacier is a glacier located in Alberto de Agostini National Park, Chile. A cascade from the glacier tumbles into the Beagle Channel.

Rink Glacier (; ) is a glacier in Avannaata, Greenland. This glacier is named in honor of Hinrich Johannes Rink, Danish geologist and Greenlandic researcher.

Closer view of the glacier in the winter A glacier cave under Mendenhall Glacier Mendenhall Glacier (also Sitaantaagu) is a glacier about long located in Mendenhall Valley, about from downtown Juneau in the southeast area of the U.S. state of Alaska. The glacier and surrounding landscape is protected as part of the Mendenhall Glacier Recreation Area, a federally designated unit of the Tongass National Forest. The Juneau Icefield Research Program has monitored the outlet glaciers of the Juneau Icefield since 1942, including Mendenhall Glacier. The glacier has also retreated since 1929, when Mendenhall Lake was created, and over since 1500.

The USGS operates a long-term "benchmark" glacier monitoring program which is used to examine climate change, glacier mass balance, glacier motion, and stream runoff. This program has been ongoing since 1965 and has been examining three glaciers in particular. Gulkana Glacier in the Alaska Range and Wolverine Glacier in the Coast Ranges of Alaska have both been monitored since 1965, while the South Cascade Glacier in Washington State has been continuously monitored since the International Geophysical Year of 1957. This program monitors one glacier in each of these mountain ranges, collecting detailed data to understand glacier hydrology and glacier climate interactions.

View from the Eielson Visitor Center, Denali Nation Park Muldrow Glacier, also known as McKinley Glacier, is a large glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates from the Great Icefall of Harper Glacier on the east side of Denali. The glacier moves generally eastwards, receiving Traleika Glacier and Brooks Glacier as tributaries, then turning north to emerge from the Alaska Range as the source of the McKinley River. Muldrow Glacier was named by Alfred Hulse Brooks in 1902 in honor of U.S. Geological Survey topographer Robert Muldrow.

Clarence Island seen from northeast with (left to right) Cape Bowles; Dobrodan Glacier and Highton Glacier surmounted by Urda Ridge; Treskavets Glacier, Orcho Glacier and Banari Glacier surmounted by Ravelin Ridge; and Cape Lloyd Dobrodan Glacier (, ) is the 3.4 km long and 1.2 km wide glacier on the east side of Urda Ridge on Clarence Island in the South Shetland Islands, Antarctica situated south of Highton Glacier. It drains the slopes of Mount Irving and Duclos-Guyot Bluff, flows northeastwards and enters the Southern Ocean south of Lebed Point. The glacier is named after the settlement of Dobrodan in Northern Bulgaria.

Dusty Glacier is located on northeast slopes of Glacier Peak in the U.S. state of Washington. The glacier descends from to and in places along its length is connected to North Guardian Glacier which lies to its south and Ermine Glacier to the north. As is true with all the glaciers found on Glacier Peak, Dusty Glacier is retreating. During the Little Ice Age, Dusty Glacier extended down to an altitude of , but since approximately the year 1850, the glacier has been in a general state of retreat and has lost more than of its length.

Gorichane Glacier (, ) is the 4.5 km long and 1.7 km wide glacier on Brabant Island in the Palmer Archipelago, Antarctica, situated east-southeast of Palilula Glacier, southwest of the head of Paré Glacier, west-northwest of the head of Laënnec Glacier, northwest of the head of Malpighi Glacier and north of Djerassi Glacier. It drains the west slopes of central Stribog Mountains and flows southwestwards into Lanusse Bay east of Baykal Point. The glacier is named after the settlement of Gorichane in Northeastern Bulgaria.

Challenger Glacier is a tidewater glacier on the north side of Heard Island in the southern Indian Ocean. Located east of Baudissin Glacier, Challenger Glacier is wide and flows into the eastern side of Corinthian Bay, close west to Saddle Point. To the east of Challenger Glacier is Downes Glacier, whose terminus is located at Mechanics Bay, between Saddle Point and Cape Bidlingmaier. To the west of Challenger Glacier is Baudissin Glacier, whose terminus is located at the western side of Corinthian Bay, near Sealers Cove.

Schmidt Glacier () is a glacier, 0.7 nautical miles (1.3 km) long, flowing west from Baudissin Glacier between Mount Drygalski and North West Cornice, on the west side of Heard Island in the southern Indian Ocean. To the north of Schmidt Glacier is Baudissin Glacier, whose terminus is located at the western side of Corinthian Bay, near Sealers Cove. Kildalkey Head is west of Schmidt Glacier. To the south of Schmidt Glacier is Vahsel Glacier, whose terminus is at South West Bay, between Erratic Point and Cape Gazert.

Map of Sentinel Range. Burdenis Glacier (, ) is the 6 km long and 1.7 km wide glacier on the east side of the main crest of north-central Sentinel Range in Ellsworth Mountains, Antarctica. It is situated north of Delyo Glacier and south of Gerila Glacier. The glacier drains the north slopes of Mount Viets and the southeast slopes of the southern summit of Long Gables Peak, flows northeastwards and together with Delyo Glacier and Gerila Glacier joins upper Ellen Glacier north of Bruguière Peak.

Stanton Glacier is in Flathead National Forest in the U.S. state of Montana. The glacier is situated in a cirque on the northeast slope of Great Northern Mountain (). Stanton Glacier is one of several glaciers that have been selected for monitoring by the U.S. Geological Survey's Glacier Monitoring Research program, which is researching changes to the mass balance of glaciers in and surrounding Glacier National Park (U.S.). Stanton Glacier is northwest of Grant Glacier.

Arapaho Glacier is an alpine glacier in a cirque immediately southeast of North Arapaho Peak, in Roosevelt National Forest in the U.S. state of Colorado. The glacier is just east of the Continental Divide. Arapaho Glacier is the largest glacier in the state of Colorado and helps provide water for the city of Boulder, Colorado. The glacier has a negative glacier mass balance and lost over 52% of its surface area during the 20th Century.

Ralitsa Glacier (, ) is the 5.5 km long and 3.5 km wide glacier on Brabant Island in the Palmer Archipelago, Antarctica, situated south of Oshane Glacier, southwest of Lister Glacier, northwest of the head of Paré Glacier and north of Palilula Glacier. It drains the northwest slopes of Mount Rokitansky in Stribog Mountains, and flows northwestwards into Guyou Bay. The glacier is named after the settlements of Ralitsa in Northeastern and Southern Bulgaria.

Baby Glacier is a glacier located in the U.S. state of Montana in Glacier National Park. Baby Glacier is situated in a cirque on the northeast slope of Numa Peak at an elevation between and above sea level. The glacier covers approximately and does not meet the threshold of often cited as being the minimum size to qualify as an active glacier. Between 1966 and 2005, Baby Glacier lost a third of its surface area.

Location of Fallières Coast on the Antarctic Peninsula. Kashin Glacier (, ) is the 8 km long and 2.7 km wide glacier on Fallières Coast in Graham Land, Antarctica. It is situated southwest of Perutz Glacier, north of Marvodol Glacier and east-southeast of Bader Glacier, flows northward between Shapkarev Buttress and Rudozem Heights, and flows into Bourgeois Fjord next southwest of Perutz Glacier. The glacier is named after the settlement of Kashin in Northern Bulgaria.

Location of Loubet Coast on the Antarctic Peninsula. Narezne Glacier (, ) is the 7 km long and 2.2 km wide glacier on Loubet Coast in Graham Land, Antarctica situated on the west side of Avery Plateau south of Field Glacier, northwest of the head of Finsterwalder Glacier and north of Haefeli Glacier. It flows northwestwards and joins Field Glacier west of Barziya Peak. The glacier is named after the cave of Narezne in Northwestern Bulgaria.

Gorkiy Peak from South Engilchek Glacier Engilchek Glacier (, - Enilchek, also Иныльчек - Inylchek) is a glacier in the Central Tian Shan Mountains of Issyk- Kul Region, northeastern Kyrgyzstan. Its snout is 50 km east of the village of Engilchek. The South Engilchek Glacier ranks as the sixth longest non-polar glacier in the world and is the largest and fastest moving glacier in Kyrgyzstan. The main glacier has two arms, the North and South Engilchek Glaciers.

On the eastern side it stands between Bamchu Glacier and Mangraon Glacier. Both these glacier's joins Milam Glacier further east, from the snout of Milam glacier emerges Goriganga River that later joins the Kali River at Jauljibi. On the western side Uttari Nanda Devi Glacier joins Uttari Rishi Glacier and drains into Rish Ganga. Rishi Ganga met with Dhauliganga River near Rini.

Rainbow Glacier is located on the northeast slopes of Mount Baker in the North Cascades of the U.S. state of Washington. Rainbow Glacier descends to nearly to the north of Lava Divide. In the middle of its course, Rainbow Glacier is connected to Park Glacier to its south and Mazama Glacier to the west. Between 1850 and 1950, Rainbow Glacier retreated .

Muir Glacier is a glacier in Glacier Bay National Park and Preserve in the U.S. state of Alaska. It is currently about wide at the terminus. As recently as the mid-1980s the glacier was a tidewater glacier and calved icebergs from a wall of ice 90 m (200 feet) tall. Photograph of Muir Glacier by Frank La Roche ca.

The Harvard Glacier is a large tidewater glacier in the Alaska's Prince William Sound. The glacier has a 1.5-mile (2 km) wide face where it calves into the College Fjord. It is 300 ft thick and covers 120,000 acres of Chugach National Forest. The Harvard Glacier is the second largest glacier in the Prince William Sound, after the Columbia Glacier.

It stands at the head of the western side of Mangraon Glacier. The glacier flows from west to east and joins Milam Glacier. Further down south east from the snout of Milam glacier emerges Goriganga River that later joins the Kali River at Jauljibi. On the western side Uttari Rishi Glacier joins Uttari Nanda Devi Glacier and drains into Rish Ganga.

Taylor Glacier is a small cirque glacier in Rocky Mountain National Park in the U.S. state of Colorado. Taylor Glacier is on the east side of the Continental Divide and adjacent to Taylor Peak. Taylor Glacier is both an ice and a rock glacier, with the lower portions of the glacier being composed primarily of rock debris and a small portion of ice.

Shanklin Glacier () is a glacier in the Hughes Range of Antarctica, flowing southeast from Mount Waterman to enter Muck Glacier at a point west of Ramsey Glacier. The glacier was named by Advisory Committee on Antarctic Names (US- ACAN) for CWO David M. Shanklin of the U.S. Army Aviation Detachment which supported the Texas Tech Shackleton Glacier Expedition, 1964–65.

Oshane Glacier (, ) is the 3 km long and 2.5 km wide glacier on Brabant Island in the Palmer Archipelago, Antarctica, situated south of Dodelen Glacier, west of Lister Glacier and north of Ralitsa Glacier. It drains the west slopes of Cushing Peak in Stribog Mountains, and flows westwards into Guyou Bay. The glacier is named after the settlement of Oshane in Northwestern Bulgaria.

Brooks Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates on the east face of Mount Silverthrone at Brooks Gap. The glacier moves northeast, joining Muldrow Glacier between Mount Brooks and Ragged Peak. Brooks Glacier was named by T.G. Gerdine of the U.S. Geological Survey circa 1900 for geologist Alfred Hulse Brooks.

Klawatti Glacier is located on the east slopes of Klawatti Peak, North Cascades National Park, in the U.S. state of Washington. The glacier is approximately in length, in width at its terminus and descends from , where it terminates above Klawatti Lake. Arêtes separate Klawatti Glacier from Inspiration Glacier to the southwest, McAllister Glacier to the northwest and North Klawatti Glacier to the north.

Agassiz Lakes near the confluence of Libbey Glacier and Agassiz Glacier. The agglomeration of the Agassiz Glacier is located on the southern flank of Mount Malaspina north of the Canada–United States border. The 25 km long glacier is fed by the Newton Glacier. The three kilometres-wide glacier flows initially in a southwesterly direction, later in a south-easterly direction.

A partly submerged glacier cave on Perito Moreno Glacier. The ice facade is approximately 60 m high Ice formations in the Titlis glacier cave A glacier cave is a cave formed within the ice of a glacier. Glacier caves are often called ice caves, but the latter term is properly used to describe bedrock caves that contain year-round ice.

Maclure Glacier (also McClure Glacier) is on Mount Maclure in the Sierra Nevada crest of Yosemite National Park in Tuolumne County, California, United States. The glacier is named after William Maclure. Like most glaciers in the Sierra Nevada, Maclure Glacier is a small cirque glacier that is long and covers an area of only . The mean elevation of the glacier is around .

Swachhand Bamak (Glacier) on the western side which later joins Gangotri Glacier. Maiandi Bamak (Glacier) on the southern side which also joins Gangotri glacier from there emerges Bhagirathi river one of the main tributaries of river Ganga. On the eastern side, Bhagirathi Kharak Glacier joins with Satopanth Glacier from, there emerges the Alaknanda river another main tributaries of river Ganga.

The Gangotri Glacier on the west side and Vasuki Glacier on the east side northern side are surrounded by Chaturangi Glacier and southern side guarded by Swachhhand Glacier. From the snout of Gangotri Glacier emerges Bhagirathi river also called Ganga or Ganges after it meets Alaknanda at Devpryag.

Kalabaland Glacier is 15 km in length, running NW to SE. It joins the Yankchar glacier and both together form the Shankalpa glacier, The Ralam Gad river originates from here which later joins Gori Ganga or Gori gad which originates at Milam Glacier on the west of Kalabaland glacier.

Spire Glacier is in Snoqualmie National Forest in the U.S. state of Washington and is on the west slopes of Spire Point. Spire Glacier flows generally northwest for a distance of approximately . An arête separates the glacier from Dana Glacier to the east. Spire Glacier descends from nearly .

Hoh Glacier is a glacier on Mount Olympus in the Olympic National Park in Jefferson County of the U.S. state of Washington. It is the source of the Hoh River. Hoh Glacier is the longest glacier on Mount Olympus at , though it is smaller in volume than Blue Glacier.

Moomaw Glacier is an alpine glacier in Rocky Mountain National Park in the U.S. state of Colorado. Moomaw Glacier is almost northeast of Isolation Peak and the old terminal moraine of the glacier impounds Frigid Lake.

Biferten Glacier The Biferten Glacier () is a glacier (2005) situated in the Glarus Alps in the canton of Glarus in Switzerland. In 1973 it had an area of . The glacier is located east of the Tödi.

Immediately south of Vahsel Glacier is Allison Glacier. Click here to see a map of Baudissin Glacier and the northwestern coast of Heard Island.

Immediately south of Vahsel Glacier is Allison Glacier. Click here to see a map of Schmidt Glacier and the northwestern coast of Heard Island.

Apollo Glacier () is a glacier, long, flowing northeast and joining the lower part of Aphrodite Glacier from the east coast of the Antarctic Peninsula.

Balch Glacier () is a glacier long, on the east coast of Graham Land, flowing southeast into Mill Inlet, to the south of Gould Glacier.

Deltabreen (The Delta Glacier) is a glacier at Edgeøya, Svalbard. The glacier debouches into the lagoon of Tjuvfjordlaguna, at the eastern side of Dyrdalen.

The Gangotri Glacier is on the west side, Vasuki Glacier is on the east side, and Chaturangi Glacier is on the north side. From the snout of Gangotri Glacier emerges Bhagirathi river, also called Ganga or Ganges.

Sentinel Range map. Berisad Glacier (, ) is a glacier long and wide in Veregava Ridge, central Sentinel Range in Ellsworth Mountains, Antarctica. It flows north-northwestwards from Kushla Peak to join Dater Glacier northeast of Sipey Peak.Berisad Glacier.

300px Passu Glacier is situated in the south side of Passu village. Passu Peak is situated in the back side of the glacier. This glacier is linked with Batura Glacier and many other glaciers of the region.

Nunatak Glacier (), also known as Nunatak Glacier, is a glacier in King Christian X Land, Northeast Greenland. Administratively it lies in the Northeast Greenland National Park zone. The area where the glacier flows is remote and uninhabited.

Angel Glacier The glacier is visible from the Cavell Meadows hiking trail.

They are home to many glaciers like Gangotri Glacier, Satopanth Glacier etc.

Noisy Creek Glacier is in North Cascades National Park in the U.S. state of Washington, northwest of Bacon Peak. Noisy Creek Glacier has retreated and left behind a series of small proglacial lakes. Noisy Creek Glacier descends from . A ridge separates Noisy Creek Glacier from Green Lake Glacier to the east.

West Depot Glacier is in North Cascades National Park in the U.S. state of Washington, on the north slopes of Mount Redoubt. Depot Glacier descends from . Melt from the glacier feeds into Depot Creek which flows into Chilliwack Lake. A ridge separates West Depot Glacier from Depot Glacier to the east.

In 1967-1979, the Cultural Revolution and other factors interrupted the observation. In 1982, the glacier became part of World Glacier Monitoring Service as a reference glacier. In 2010, an observation tower was built in the glacier area. In 2013, the glacier was listed among the sites for Global Cryosphere Watch.

Beowulf Glacier () is a small north-flowing glacier located between Mime Glacier and the head of Rhone Glacier in the Asgard Range, Victoria Land. It was named in 1983 by the New Zealand Antarctic Place-Names Committee from association with Mount Beowulf which stands at the head of this glacier.

Upper Curtis Glacier is in North Cascades National Park in the U.S. state of Washington, on the west slopes of Mount Shuksan. Upper Curtis Glacier is not connected to Lower Curtis Glacier downslope to the southwest, but is to Hanging Glacier to the north and to Sulphide Glacier to the east.

Debeli Namet is a small glacier below the mountain of Šljeme () in the Durmitor massif, Montenegro. This glacier exists well below the true snowline and is sustained by avalanching snow. Results of recent investigations on the Debeli Namet glacier have been published by a British scientist (Hughes 2007). The Debeli Namet glacier is not quite the southernmost glacier in Europe, as this status currently goes to the Snezhnika glacier (latitude of 41°46′09″ N) followed by Banski Suhodol Glacier also in Pirin mountain in Bulgaria and the Calderone Glacier in Italy.

Muir Inlet schematic map. Muir Inlet is an inlet in Glacier Bay, U.S.A. Muir Inlet heads in Muir Glacier, and extends for "Fjords as temporary sediment traps: History of glacial erosion and deposition in Muir Inlet, Glacier Bay National Park, southeastern Alaska" GSA Bulletin (2010) 122 (7–8): 1067–1080. south to Glacier Bay, NW of Hoonah, Alaska Muir Inlet is separated from Chilkat Inlet and Lynn Canal by Chilkat Range. Muir Inlet has several glacier's terminuses besides Muir Glacier, most prominent are Casement Glacier, McBride Glacier and Riggs Glacier.

Tributaries in the lower parts are the Rudolf Glacier, Forrest Ross Glacier, Kaufmann Glacier, Haast Glacier, Hochstetter Glacier, and Ball Glacier. The glacial terminal lake is met by the meltwater of the Murchison Glacier, which approaches from the northeast and flows alongside the Tasman Glacier outside the moraine wall. The waters of Tasman Lake flow into the Tasman River and flow south joining the Hooker River draining the proglacial lakes on the Hooker and Mueller Glaciers. The Tasman River exhibits a braided characteristic, and flows south into Lake Pukaki.

Map of northern Sentinel Range Skaklya Glacier (, ) is the long and wide glacier on the east side of the main crest of northern Sentinel Range in Ellsworth Mountains, Antarctica. It is situated northwest of Zhenda Glacier and southeast of the head of Vidul Glacier. The glacier drains the south slopes of Mount Reimer and the north slopes of Blenika Peak, flows east- northeastwards and together with Zhenda Glacier joins Sabazios Glacier west of Mount Lanning in Sostra Heights. The glacier is named after Skaklya Waterfall in Western Bulgaria.

Location of Clarence Island in the South Shetland Islands. Clarence Island seen from northeast with (left to right) Cape Bowles; Dobrodan Glacier and Highton Glacier surmounted by Urda Ridge; Treskavets Glacier, Orcho Glacier and Banari Glacier surmounted by Ravelin Ridge; and Cape Lloyd. Gesha Point (, ‘Nos Gesha’ \'nos 'ge-sha\\) is the small point on the east coast of Clarence Island in the South Shetland Islands, Antarctica separating the glacier termini of Orcho Glacier to the north and Treskavets Glacier to the south. The point is named after the settlement of Gesha in Northern Bulgaria.

Debris-covered lower slopes of Miage Glacier in 2009 The Miage Glacier (; ) is a debris-covered glacier in the upper Aosta Valley, in northwestern Italy.

From the west, the Libbey Glacier meets the Agassiz Glacier. This finally merges into the Malaspina Glacier, which finally flows into the Gulf of Alaska.

The Peters Glacier lies on the northwest side of the massif, while the Muldrow Glacier falls from its northeast slopes. Just to the east of the Muldrow, and abutting the eastern side of the massif, is the Traleika Glacier. The Ruth Glacier lies to the southeast of the mountain, and the Kahiltna Glacier leads up to the southwest side of the mountain. With a length of , the Kahiltna Glacier is the longest glacier in the Alaska Range.

Shepard Glacier is a glacier remnant (glacieret) In Glacier National Park in the U.S. state of Montana. The glacieret is immediately southeast of Cathedral Peak. Shepard Glacier was one of a number of glaciers that have been documented by the United States Geological Service (USGS) to have retreated significantly in Glacier National Park. Shepard Glacier was measured in 2009 to have decreased to less than , considered to be a minimal size to qualify as being considered an active glacier.

Butterfly Glacier is in Wenatchee National Forest in the U.S. state of Washington and is on the northwest slopes of the northwest summit of Luahna Peak and the ridge which extends west from the peak. Butterfly Glacier is separated into two glaciers, the larger one in the east descends from . An arête separates Butterfly Glacier from Pilz Glacier to the east. Butterfly Glacier is within the Glacier Peak Wilderness and is just over southeast of Glacier Peak.

Closeup of the glacier Chenega Glacier is a tidewater glacier located in Prince William Sound and on the Kenai Peninsula in the U.S. state of Alaska. Chenega Glacier was named in 1905 for Chenega Island and the nearby community of Chenega Bay. The glacier is a tourist attraction, drawing many kayakers and small cruise lines to Nassau Fjord where the glacier meets the ocean. Most individual expeditions to the glacier originate in the Prince William Sound community of Whittier.

Andrews Glacier is an alpine glacier in a cirque below Otis Peak () in Rocky Mountain National Park in the U.S. state of Colorado. The glacier extends from Andrews Pass at nearly with some perennial snow extending to Andrews Tarn, a small proglacial lake. When images of the glacier taken in the early 1900s are compared with those of the early 2000s, Andrews Glacier is showing a negative glacier mass balance which indicates the glacier is retreating.

Map of northern Sentinel Range. Zhenda Glacier (, ) is the 8 km long and 4.8 km wide glacier on the east side of the main crest of northern Sentinel Range in Ellsworth Mountains, Antarctica. It is situated west of Sabazios Glacier and southeast of Skaklya Glacier. The glacier drains the northeast slopes of Mount Sharp and the east slopes of Mount Barden, flows northeastwards and together with Skaklya Glacier joins Sabazios Glacier west of Mount Lanning in Sostra Heights.

Of the nineteen glaciers of the Juneau Icefield, eighteen are retreating, and one, the Taku Glacier, is advancing. Eleven of the glaciers have retreated more than since 1948 — Antler Glacier, ; Gilkey Glacier, ; Norris Glacier, and Lemon Creek Glacier, . Taku Glacier has been advancing since at least 1890, when naturalist John Muir observed a large iceberg calving front. By 1948 the adjacent fjord had filled in, and the glacier no longer calved and was able to continue its advance.

The West (Pachmi or Paschimi) Kamet Glacier, the East (Purbi or Purva) Kamet Glacier and the Raikana Glacier systems surround Kamet. The branches of the West Kamet Glacier head on the western slopes of Kamet, Abi Gamin, and Mukut Parbat. The East Kamet Glacier flows from the eastern side of Kamet and Mana. The Raikhana glacier originates on the east side of Meade's Col saddle, flows east of Abi Gamin, and unites with the East Kamet Glacier.

Due to the advance, two lobes of the glacier joined together in late May 2008 and thus the glacier completely surrounds the lava domes. – Glacier is still connected south of the lava dome. – Glacier arms touch on North end of glacier. In addition, since 2004, new glaciers have formed on the crater wall above Crater Glacier feeding rock and ice onto its surface below; there are two rock glaciers to the north of the eastern lobe of Crater Glacier.

Glasiologbreen ("glaciologist glacier") is a glacier in Torell Land at Spitsbergen, Svalbard. The glacier has a length of five kilometers, and is situated between the mountains of Gerdnuten and Wijkberget. Glasiologbreen is part of the Liestølbreen glacier complex.

Prouty Glacier is located in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation generally between . Prouty Glacier is on the northeast slopes of South Sister, a dormant stratovolcano. Beyond the current range of the glacier, glacially formed Carver Lake lies to the immediate northeast of Prouty Glacier and is impounded by the old terminal moraine of the glacier.

Location of Pernik Peninsula on Loubet Coast, Antarctic Peninsula. Dolie Glacier (, ) is the 9.5 km long and 2.4 km wide glacier on Pernik Peninsula, Loubet Coast in Graham Land, Antarctica, situated southwest of McCance Glacier and northeast of Blagun Glacier. It flows northwestwards between Hodge Ridge and Liebig Peak, and joins Wilkinson Glacier. The glacier is named after the settlement of Dolie in Southern Bulgaria.

Dodelen Glacier (, ) is the 3.6 km long and 2.8 km wide glacier on Pasteur Peninsula, Brabant Island in the Palmer Archipelago, Antarctica, situated southwest of Podayva Glacier, northwest of Lister Glacier and north of Oshane Glacier. It drains the west slopes of Mount Hunter in Stribog Mountains, and flows westwards into Guyou Bay. The glacier is named after Dodelen River in eastern Balkan Mountains.

Logan Glacier is in Glacier National Park in the U.S. state of Montana. The glacier is situated in a cirque to the northeast of Mount Logan. Just east of the Continental Divide, Logan Glacier is northwest of Red Eagle Glacier. Estimated in 2005 to cover an area of , Logan Glacier covered almost in 1966, a reduction in area of 40 percent in about 40 years.

The south side, however, does have some perennial snowfields on its slopes. The Crescent Glacier is the source of Morrison Creek; and, although it does not feed it directly, the Gotchen Glacier is the source of Gotchen Creek. Both creeks drain to the White Salmon River. The rugged east side has four glaciers, the Mazama Glacier, Klickitat Glacier, Rusk Glacier, and the Wilson Glacier.

Tokositna Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates in two major arms on the east side of Mount Hunter, moving east until the main arms join, then turning south. Tokositna Glacier is the source of the Tokositna River. Spelling variants and alternate names include Tokasitna Glacier, Tokichitna Glacier and Tuqashitnu Li'a.

Bara Shigri is the largest glacier located in the state of Himachal Pradesh, India, Bara-Sigri glacier which is the second longest glacier in Himalaya (Indian side) after Gangotri, both are around 30 km long. The glacier is located in the Chandra Valley of Lahaul. The glacier feeds the Chenab River. The name comes from the Lahaul dialect, where Bara means big and Shigri means glacier.

Gould Glacier () is a glacier, long, on the east coast of Graham Land, Antarctica, flowing south-east into Mill Inlet, to the west of Aagaard Glacier. It was first surveyed by the Falklands Islands Dependencies Survey in 1946–47, and named "East Gould Glacier". Together with "West Gould Glacier" it was reported to fill a transverse depression across Graham Land, but further survey in 1957 showed that there is no close topographical alignment between the two. The name Gould Glacier, after Rupert T. Gould, a British polar historian and cartographer, is now only applied to this glacier, and the west glacier is now called Erskine Glacier.

Hidden crevasses have led to the deaths of unprepared tourists. Athabasca Glacier tour in 2006 Athabasca Glacier snow coach in 2009 Terra Bus on the Athabasca Glacier in 2010 Approaching Athabasca Glacier Headwall Athabasca Glacier headwall (on the ramp) The Icefield Interpretive Centre, closed during the winter (mid-October to mid-April),Columbia Icefield 2007 tour brochure stands across from the glacier. It is used as a lodge and for ticket sales for sightseeing on the glacier. Standard buses transport tourists to the glacier edge, where they board specially designed snow coaches for transport over the steep grades, snow and ice part way up the glacier.

Sona glacier and Meola glacier serves the route to climb Panchchuli peaks from east facing direction. Sona glacier is situated north to Meola Glacier. It is situated just below peaks like Ngalaphu 6,410 m and Panchchuli I.It is divided into Upper and Lower.The direction of the glacier is south west to north east.

Kjerulf Glacier () is a glacier in Jan Mayen. It begins at the Hakluyttoppen slope, in the outer crater edge of the Beerenberg. The Kjerulf Glacier and both its neighbors, the Weyprecht Glacier in the west and the Svend-Foyn Glacier in the east, are the most active glaciers in the island.Robert P. Sharp.

It is gradual climb. Vasuki Parvat (4800 m) : Hike up the moraines of the Gangotri Glacier after which a climb up to the Ghaumk glacier to the east begins. South of this glacier lie a few meadows named Vasuk Parvat. Glacier camp (5200 m) : A streneous climb over the morained filled glacier.

Glacier Country, Montana is a tourism region in the U.S. state of Montana. Glacier Country includes the cities of Missoula, Kalispell, Polson, Libby, Whitefish, Browning, Eureka, and Thompson Falls. Glacier Country is home to Glacier National Park, and Montana's 2nd largest city- Missoula, Montana. The 2015 population of Glacier Country is 332,702.

The Llewellyn Glacier is a glacier located in British Columbia. It is the second-largest glacier in the Juneau Icefield. The glacier has rapidly retreated as of recent, and on June 6, 2018, a large kilometre-sized chunk of the narrow tongue of the glacier broke off and plunged into Atlin Lake.

The Gorodetsky Glacier is a rock glacier on the Northern slope of the Zailiysky Alatau range. The glacier consists of left and right branches. The glacier was visited by dendrologist and archaeologist Vladimir Dmitrievich Gorodetsky (1878–1943) the first time in 1916. The glacier was named in honor of Gorodetsky 20 years later.

Skinner Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation near , just west of Carver Glacier. Skinner Glacier is on the north slopes of South Sister, a dormant stratovolcano.

Carver Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation near , just east of Skinner Glacier. Carver Glacier is on the north slopes of South Sister, a dormant stratovolcano.

Yawning Glacier is in North Cascades National Park in the U.S. state of Washington, on the east slopes of Magic Mountain. Yawning Glacier descends from . S Glacier lies to the south and Cache Col Glacier is to the northwest.

Alsek Glacier is a long glacier in Glacier Bay National Park in the Panhandle of Alaska (USA). Alsek Glacier MapCarta The name Alsek is of Tlingit origin and may mean "place where people rest". Alsek River. The Canadian Encyclopedia.

Ambulapcha Glacier is a glacier of the Himalayas in the Solukhumbu District of Nepal. It adjoins Imja Glacier to its south and with Lhotse Shar Glacier forms three major glaciers. It forms the Ambulapcha Tsho glacial lake, located at .

Rippon Glacier is a small glacier located in Kemp Land, East Antarctica. It is close east of Seaton Glacier, flowing southward into Edward VIII Ice Shelf.

Snowbird Glacier is a hanging alpine glacier in the Talkeetna Mountains of Alaska.

Garden Glacier is separated by an arête from Chickamin Glacier to the north.

Mount Everest is the source of the Rongbuk Glacier and East Rongbuk Glacier.

Ramani Glacier on the northern side and Rishikot Glacier and Changabang Glacier on the eastern side. All these glacier drains into Rish Ganga. Rishi Ganga met with Dhauli ganga near Rini. Later Dhauli ganga met with Alaknanda at Vishnu Pryag.

Cache Col Glacier is in North Cascades National Park in the U.S. state of Washington, on the east slope of Mix-up Peak. Cache Col Glacier retreated nearly between 1950 and 2005. Cache Col Glacier is northwest of Yawning Glacier.

Fair Glacier is an alpine glacier located just west of Apache Peak, in Roosevelt National Forest in the U.S. state of Colorado. The glacier is immediately west of the Continental Divide on the opposite side of the divide from Isabelle Glacier.

Sunrise Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates near Scott Peak, moving northwest. It is the source of Sunrise Creek. Sunset Glacier is nearby.

The Diablerets Glacier () is a glacier situated on the summit of Les Diablerets in the Bernese Alps. It covers an area of approximatively 1 km2. The Diablerets Glacier is often confused with the nearby much larger and popular Tsanfleuron Glacier.

Near by glaciers and river Dakshini Chamrao glacier, Balbala glacier and Paschimi Kamet glacier all the glacier drain their water in the Saraswati river which then joins Alaknanda River near Mana village one of the main tributaries of Ganga river.

The Rogers massif includes five individually-named summits: Rogers Peak, Grant Peak, Fleming Peak, Swiss Peak, and Truda Peaks.Mount Rogers BC Geographical Names Numerous glaciers radiate from all sides, including the Rogers Glacier, Swiss Glacier, Tupper Glacier, and Hermit Glacier.

Particular attention was paid to the glacier Central Tuyuksu, which became a representative glacier of the World Glacier Monitoring Service for the Central Asian region. Thanks to his efforts, constant research on the Central Tuyuksu Glacier has been carried out since 1956 to the present. The series "Fluctuations of Glaciers", issued every 5 years, are available on the World Glacier Monitoring Service website. The website also offers "Glacier Mass Balance Bulletin" as well as the "Global Glacier Change Bulletin", published biennially.

White Chuck Glacier is located in the Glacier Peak Wilderness in the U.S. state of Washington and is south of Glacier Peak. The glacier is within Mount Baker-Snoqualmie National Forest and nearly touches the White River Glacier though they are separated by an arête off the Kololo Peaks. White Chuck Glacier has retreated significantly since the end of the Little Ice Age. From about 1850 to 1930, the glacier thinned and by 1940, a fast rate of retreat commenced.

Stephenson Glacier () is a glacier close west of Dovers Moraine on the east side of Heard Island in the southern Indian Ocean. Its terminus is between Dovers Moraine and Stephenson Lagoon, with part of the glacier flowing to Doppler Hill and Sealers Beach. To the north of Stephenson Glacier is Brown Glacier, whose terminus is located at Brown Lagoon. To the southwest of Stephenson Glacier is Winston Glacier, whose terminus is located at Winston Lagoon, between Cape Lockyer and Oatt Rocks.

Map of northern Sentinel Range. Anchialus Glacier (, ) is the 8.5 km long and 3.4 km wide glacier in Sostra Heights on the east side of northern Sentinel Range in Ellsworth Mountains, Antarctica. It is situated north of lower Embree Glacier, east of Sabazios Glacier, south of lower Newcomer Glacier and northwest of Vit Ice Piedmont. The glacier drains the northeast slopes of Mount Malone and the west slopes of Bracken Peak, flows northwards and joins Newcomer Glacier east of Mount Lanning.

Columbia Glacier in 2004 The calving rate will increase as the glacier retreats from the shoal into the deeper fjord just cleared by the glacier during advance. The water depth initially increases as the glacier retreats from the shoal, causing every more rapid glacier flow, calving and retreat. A glacier is comparatively insensitive to climate during this calving retreat. However, in the case of San Rafael Glacier, Chile, a switch from retreat (1945–1990) to advance (1990–1997) was noted.

Wright Lower Glacier () is a stagnant glacier occupying the mouth of Wright Valley and coalescing at its east side with Wilson Piedmont Glacier, in Victoria Land. The glacier was originally called "Wright Glacier" by the British Antarctic Expedition (1910–13), for expedition member C.S. Wright. The name was adjusted decades later by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1958–59), when the VUWAE also defined the name Wright Upper Glacier for the separate glacier at the head of Wright Valley.

Harrison Glacier is located in the US state of Montana in Glacier National Park. Situated on a southeast facing ridge immediately south of Mount Jackson, Harrison Glacier is the largest glacier in Glacier National Park and was estimated in 2005 to have an area of . Though many experts have stated that all the glaciers in Glacier National Park may disappear by the year 2030, Harrison Glacier lost only 9 percent of its surface area in the 40-year period between 1966 and 2005 and will likely still exist well beyond 2030. Compared to many of the vanishing glaciers in Glacier National Park, Harrison Glacier has a much higher altitude accumulation zone (approximately ) which has allowed it to maintain some equilibrium in its glacier mass balance.

McElroy Glacier is a tributary glacier just west of Matthews Ridge on Tapsell Foreland in Victoria Land. It drains to the south to join nearby Barnett Glacier.

Smoot pp. 93–97 The peak supports three glaciers including Banded Glacier to the north, Fremont Glacier to the southwest and Douglas Glacier on the southeast slopes.

Peary Glacier (), is a glacier in NW Greenland. Administratively it belongs to the Avannaata municipality. This glacier was named after US Arctic explorer Robert Peary (1856 - 1920).

The south face of Mount Vinson is drained by Roché Glacier, which flows westwards into Branscomb Glacier, with the latter leaving Vinson Massif to join Nimitz Glacier.

Aiken Glacier () is a small glacier between Von Guerard Glacier and Wales Glacier on the north slope of Kukri Hills, Victoria Land. It was named by the Advisory Committee on Antarctic Names (1997) from association with Aiken Creek, named for USGS Hydrologist Dr. George R. Aiken, which flows north from this glacier into Taylor Valley.

It occupied the center of Bennett Island; had an elevation of above mean sea level; and was thick at its center. It had an outlet glacier, West Seeberg Glacier, from which ice flowed downhill from Toll Glacier into the sea. The next largest glacier was De Long East Glacier with an area of in 1987.

It is surrounded by Glaciers on the three side Changabang Glacier,on the southern side, Uttari Rishi Glacier On the eastern side and Bagini Glacier on the northern side. The River from Bagini Glacier met with Dhauli Ganga at Jumma. Changabang Bamak (Glacier) and Uttari Rishi Bamak (Glacier) also met Dhauli Ganga through Rishi Ganga gorge. later Dhauli Ganga met with Alaknanda river at Vishnu Prayag two main tributaries of Ganga.

Mazama Glacier is located on Mount Baker in the North Cascades of the U.S. state of Washington. Between 1850 and 1950, Mazama Glacier retreated . During a cooler and wetter period from 1950 to 1979, the glacier advanced but between 1980 and 2006 retreated back . Situated on the north slopes of Mount Baker, Mazama Glacier is bordered by the Park Glacier to the south and Rainbow Glacier to the east.

Belogradchik Glacier (, ) is a 14 km long and 5.6 km wide glacier in the southern Aristotle Mountains on Oscar II Coast in Graham Land, Antarctica, situated south of Jeroboam Glacier and west of Ambergris Glacier. It drains from the southeast slopes of Madrid Dome and flows southeastwards to join Flask Glacier east of Mount Fedallah. The feature is named after the town of Belogradchik in northwestern Bulgaria.Belogradchik Glacier.

Boryana Glacier (, ) is the 11 km long and 3.2 km wide glacier on Nordenskjöld Coast in Graham Land, Antarctica situated west-southwest of Desudava Glacier and northeast of Darvari Glacier. It is draining the southeast slopes of Detroit Plateau, flowing between Rice Bastion and Gusla Peak, then turning southwards to enter Mundraga Bay between Desudava Glacier and Darvari Glacier. The feature is named after the settlement of Boryana in northeastern Bulgaria.

There are many glaciers in the Pamir Mountains, including the long Fedchenko Glacier, the longest in the former USSR and the longest glacier outside the polar regions.In the Karakoram Mountains, Siachen Glacier is 76 km long, Biafo Glacier is 67 km long, and Baltoro is 63 km long. The Bruggen or Pio XI Glacier in southern Chile is 66 km long. Kyrgyzstan's South Inylchek (Enylchek) Glacier is 60.5 km in length.

Dixon Glacier is located in the U.S. state of Montana in Glacier National Park. The glacier is situated in a cirque immediately to the north of The Sentinel at an elevation between and above sea level. Immediately east of the Continental Divide, the glacier is east of Thunderbird Glacier. Dixon Glacier covers an area of approximately and between 1966 and 2005 lost over 45 percent of its surface area.

Then the glacier flows to the south-east towards the Aletsch Glacier without reaching it. The glacier tongue ends at around . During the Little Ice Age in the middle of the 19th century the glacier was part of the Aletsch Glacier. The Swiss Alpine Club Oberaletschhütte () is above the junction of the two glacier arms and has been accessible to hikers since 2005 with a new trail from Belalp.

Chuchuliga Glacier (, ) is the 14 km long and 12 km wide glacier on Oscar II Coast, Graham Land in Antarctica situated southwest of Dzhebel Glacier, northeast of Stob Glacier and south-southeast of Archer Glacier. It is draining from the slopes of Bruce Plateau, and flowing south-southeastwards to join Crane Glacier.Chuchuliga Glacier SCAR Composite Antarctic Gazetteer The feature is named after the settlement of Chuchuliga in southern Bulgaria.

The glacier once contained ice caves in the smooth ice before the 2004-2008 volcanic activity. The growth of the lava dome and volcanic eruptions from 2004 to 2008 significantly altered the appearance of the glacier. In the same time period, several agencies decided to put an official name on the glacier which, at first, was Tulutson Glacier. A later decision made Crater Glacier the official glacier name.

Rotunda Glacier () is a tributary glacier flowing north between Ugolini Peak and La Count Mountain into upper Ferrar Glacier, Victoria Land. The name Rotunda Glacier was used for this feature in the report "Tephra in Glacier Ice" by J.R. Keys, P.W. Anderton, and P.R. Kyle following the 1973-74 and 1974-75 seasons. Named in association with the butte of the same name on the west side of the glacier.

Brown Glacier () is a glacier just south of Round Hill on the east side of Heard Island in the southern Indian Ocean. Its terminus is at Brown Lagoon. To the northwest of Brown Glacier is Compton Glacier, whose terminus is located at Compton Lagoon, between Gilchrist Beach and Fairchild Beach. To the southeast of Brown Glacier is Stephenson Glacier, whose terminus is located between Dovers Moraine and Stephenson Lagoon.

Deacock Glacier () is a glacier close west of Lavett Bluff on the south side of Heard Island in the southern Indian Ocean. Its terminus is between Cape Labuan and Long Beach. To the east of Deacock Glacier is Fiftyone Glacier, whose terminus is located between Lavett Bluff and Lambeth Bluff. To the west of Deacock Glacier is Gotley Glacier, whose terminus is located between Cape Arkona and Cape Labuan.

Winston Glacier () is a glacier flowing to Winston Lagoon on the southeast side of Heard Island in the southern Indian Ocean. Its terminus is at Winston Lagoon, between Cape Lockyer and Oatt Rocks. To the northeast of Winston Glacier is Stephenson Glacier, whose terminus is located between Dovers Moraine and Stephenson Lagoon. To the southwest of Winston Glacier is Fiftyone Glacier, whose terminus is located between Lavett Bluff and Lambeth Bluff.

Fiftyone Glacier is a large glacier flowing southwards, on the south side of Heard Island in the southern Indian Ocean. Its terminus is located between Lavett Bluff and Lambeth Bluff. To the northeast of Fiftyone Glacier is Winston Glacier, whose terminus is located at Winston Lagoon, between Cape Lockyer and Oatt Rocks. To the west of Fiftyone Glacier is Deacock Glacier, whose terminus is located between Cape Labuan and Long Beach.

Thamyris Glacier (, ) is a 3 km long and 2.8 km wide glacier draining the east slopes of the Trojan Range on Anvers Island in the Palmer Archipelago, Antarctica. Situated east of Iliad Glacier, south of Rhesus Glacier and northwest of Kleptuza Glacier. Flowing northeastwards into Fournier Bay south of Predel Point and north of Madzharovo Point. The glacier is named after the Thracian singer Thamyris in Homer's Iliad.

North Klawatti Glacier lies in a cirque to the east of Austera Peak, North Cascades National Park, in the U.S. state of Washington. The glacier is approximately in length, in width at its widest and descends from , where it terminates above Klawatti Lake. An arête divides North Klawatti Glacier from Klawatti Glacier to the south. The North Klawatti Glacier was one of four glaciers selected for glacier mass balance research.

Zemu Glacier remains a less studied and monitored glacier. Studying digital imagery shows that the glacier has receded 27 meters every year between 1967–1984. The retreat is not massive given the great length of the glacier. There is a thick layer of debris on the glacier, preventing ablation: there are, however, small lakes that have formed on the surface of these debris-covered sections of the glacier.

Map of Sentinel Range. Padala Glacier (, ) is the long and wide glacier in Bangey Heights on the east side of the main ridge of north-central Sentinel Range in Ellsworth Mountains, Antarctica. It is situated northwest of Kopsis Glacier and east-southeast of Marsa Glacier. The glacier drains the northeast slopes of Bezden Peak and the southeast slopes of Golemani Peak, flows northeastwards and joins Embree Glacier northwest of Mount Hleven.

Middle Cascade Glacier is in Wenatchee National Forest in the U.S. state of Washington and is to the north of Spider Mountain and east of Mount Formidable. Middle Cascade Glacier has a significant icefall that is thinning and may eventually separate the upper section of the glacier from the lower. Middle Cascade Glacier retreated between 1979 and 2005. The smaller Spider Glacier is just southeast of Middle Cascade Glacier.

Spider Glacier is in Wenatchee National Forest in the U.S. state of Washington and is to the north of Spider Mountain. Spider Glacier is long and extends for across the north face of Spider Mountain. Spider Glacier is separated by an arête from Middle Cascade Glacier to the west. This Spider Glacier is not to be confused with another of the same name nearby, Spider Glacier (Phelps Ridge, Washington).

The Raktvarn Glacier. that met with Gangotri Glacier from there emerge the Bhagirathi river.

It was what remained of an earlier glacier known as the Little Barranco Glacier.

Midgard Glacier () is a glacier on the east coast of the Greenland ice sheet.

Hainablak Glacier is a glacier near Trango Tower mountain in Baltistan, Gilgit-Baltistan, Pakistan.

Penny Royal Glacier is a hanging alpine glacier in the Talkeetna Mountains of Alaska.

Of all the great glaciers in the Oisans region, the Glacier Noir is the one that descends furthest into the valley. This is thanks to favourable topography and the fact that the lower tongue of the glacier is entirely covered with ablation moraine. As a result, it is better screened from direct sunshine than, for example, its neighbour, the Glacier Blanc ("white glacier"). Until at least 1866 the Glacier Noir and Glacier Blanc were combined into a single glacial systemAccording to other sources the separation of the Glacier Blanc and the Glacier Noir occurred in 1876, c.f.

The Lower Grindelwald Glacier () is a Glacier in the Swiss Bernese Alps, situated to the south-east of Grindelwald. It starts below the Agassizhorn and the Strahlegghörner and is connected with the Finsteraar Glacier via the Finsteraarjoch (). The top of the glacier below the Finsteraarhorn in the back and Agassizhorn to the right (August 2008) The Lower Grindelwald Glacier yet has a major tributary, the Ischmeer (Swiss German for Ice Sea, formerly known as Grindelwald-Fiescher Glacier, ), which is the glacier overlooked by the Jungfrau Railway's Eismeer railway station. The Lower Grindelwald Glacier was about long and covered an area of in 1973.

Huntress Glacier from Willan Saddle. Topographic map of Livingston Island and Smith Island. Huntress Glacier is a glacier long and wide flowing into the head of False Bay, Livingston Island in the South Shetland Islands, Antarctica. It is situated east of Johnsons Glacier, southeast of Contell Glacier and Balkan Snowfield, south of upper Perunika Glacier, southwest of Huron Glacier and northwest of Macy Glacier, and is bounded by Friesland Ridge and the Tangra Mountains to the southeast, Nesebar Gap, Pliska Ridge, Burdick Ridge and Willan Nunatak to the north, and Charrúa Gap and Napier Peak to the northwest.

The Gangotri Glacier on the east side and Vasuki Glacier on the west side. From the snout of Gangotri Glacier emerges Bhagirathi river also called Ganga or Ganges.

The Glacier Noir (French for "black glacier") is a glacier in the Massif des Écrins in the French Alps. It is located in the département of Hautes-Alpes.

It is surrounded by glaciers on all the sides: Kalindi Glacier on the southern side, Arwa Glacier on the eastern side, and Mana Glacier on the northern side.

Mill Stream Glacier () is a tributary glacier, about wide, flowing west between the Supporters Range and Otway Massif in Antarctica to enter Mill Glacier. It was named by the New Zealand Geological Survey Antarctic Expedition of 1961–62 in association with Mill Glacier.

Helen Glacier Tongue () is a glacier tongue which extends seaward from Helen Glacier on the coast of Antarctica. It was discovered in November 1912 by the Western Base Party of the Australasian Antarctic Expedition under Mawson, and is named after Helen Glacier.

The glacier is split into an upper and a lower part, with a non-glaciated area between. The glacier reaches down to an elevation of above sea level, the lowest glacier level in southern Norway. The Bøyabreen glacier lies just northwest of Supphellebreen.

Eugene Glacier is located in the US state of Oregon. The glacier is situated in the Cascade Range at an elevation generally above and is east of Lost Creek Glacier. Eugene Glacier is on the northwest slopes of South Sister, a dormant stratovolcano.

One of the caves leading to the glacier base. Russell Glacier () is a glacier in the Qeqqata municipality in central-western Greenland. It flows from the Greenland ice sheet () in the western direction. The front of the glacier is located east of Kangerlussuaq.

Hidden Glacier is located in the US state of Montana. The glacier is situated in the Beartooth Mountains at an elevation of , nestled within a cirque between Mount Villard to the east and Glacier Peak to the west. The glacier covers approximately .

Daniel Glacier is in Wenatchee National Forest in the U.S. state of Washington and is on the north slope of Mount Daniel. Daniel Glacier retreated almost between 1950 and 2005. Daniel Glacier is separated from Lynch Glacier to the west by a ridge.

Despite the volcanic activity, the glacier continued to advance and by mid-2008, the glacier completely encircled the lava domes. \- Glacier is still connected south of the lava dome. In addition, new glaciers (rock or ice) have formed around Crater Glacier as well.

Dall Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Alaska Range on Mount Russell, moving southwest, then south to the Yentna River just below the present terminus of Yentna Glacier.

Rhone Glacier is a glacier lying west of Matterhorn Glacier and flowing south toward the junction of Lake Bonney and Taylor Glacier in Victoria Land, Antarctica. It was charted and named by the British Antarctic Expedition, 1910–13, under Robert Falcon Scott.

Kronborg Glacier () is a glacier on the east coast of the Greenland ice sheet. It is named after Kronborg Castle in Denmark. Administratively this glacier is part of the Sermersooq Municipality.Google Earth The area surrounding the Kronborg Glacier is remote and uninhabited.

Overlooking Ovech Glacier to the southeast, Vetrino Glacier to the north, Yablanitsa Glacier to northwest, and Chuprene Glacier to the southwest. Bulgarian early mapping in 2009. Named after the Bulgarian scientist Marin Drinov (1838–1906), founding chairman of the Bulgarian Academy of Sciences.

Mount Carter () is located in the Livingston Range, Glacier National Park in the U.S. state of Montana. Rainbow Glacier is just south of Mount Carter while Weasel Collar Glacier is immediately northeast. Mount Carter is the tenth tallest peak in Glacier National Park.

Adishi Glacier () is a valley glacier located in the central part of the Greater Caucasus Mountain Range in the Svaneti Region of Georgia. The glacier lies on the southern slopes of the Caucasus. The length of the Adishi Glacier is and its surface area is . The tongue of the glacier descends down to above sea level.

Moa Glacier () is a valley glacier between Marr Glacier and Goldman Glacier in the Kukri Hills of Victoria Land, Antarctica. It flows north into Taylor Valley but terminates midway down the south wall of the valley. The glacier was named by the New Zealand Geographic Board in 1998 after the moa, an extinct New Zealand bird.

Silver Glacier is in North Cascades National Park in the U.S. state of Washington and descends to the northwest from near the summit of Mount Spickard. Silver Glacier descends from , and Silver Lake lies below the current terminus of the glacier. The National Park Service is currently studying Silver Glacier as part of their glacier monitoring project.

Glacier Falls is a cascade located in Glacier Gulch, Grand Teton National Park in the U.S. state of Wyoming. The cascade drops approximately in Glacier Gulch, fed by runoff from the Teton Glacier. More than a below Delta Lake, Glacier Falls is a highly intermittent waterfall that is usually at peak flow during late spring and early summer snowmelt.

Dana Glacier is in Wenatchee National Forest in the U.S. state of Washington and is west of Dome Peak. Dana Glacier flows generally north for a distance of approximately . An arête divides the glacier in two while other aretes separate Dana Glacier from Chickamin and Dome Glaciers to the east and south respectively. Dana Glacier descends from nearly .

Ever since then, the glacier has been continuously retreating. Due to its constant recession, the glacier has been separated into two branches in 1993. The glacier is one of the 'reference glaciers' for mass balance of the World Glacier Monitoring Service (WGMS). In 2019, researchers estimated that the glacier will have disappeared in the next 50 years.

Raikana Glacier, Uttari Raikana Glacier, Ganesh Glacier all three glacier joins Purbi Kamet Glacier from there emerges the river Dhauli Ganga which met Alaknanda river at Vishnu Prayag an 82 km journey from its mouth. Alaknanda river is one of the main tributaries of river Ganga which later joins the other tributaries Bhagirathi river at Dev Prayag.

American Glacier is located in the Bridger Wilderness of Bridger-Teton National Forest, in the U.S. state of Wyoming. Descending from the east slope of American Legion Peak, the glacier elevation ranges from . American Legion Glacier is just west of Twins Glacier and east of Stroud Glacier and is at the head of the valley known as Titcomb Basin.

Richardson Glacier is in Wenatchee National Forest in the U.S. state of Washington and is on the south slopes Luahna Peak and north slopes of Clark Mountain. Richardson Glacier descends from . Richardson Glacier is connected to Clark Glacier to the east at its upper margins. Richardson Glacier is named after J.B. Richardson, an early settler to the region.

Shelf Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Kichatna Mountains on the side of Kichatna Spire, moving north. It is a tributary to neighboring Shadows Glacier, which with Cul-de-sac Glacier feeds the west fork of the Yentna River.

Forbidden Glacier is on the north slopes of Forbidden Peak, North Cascades National Park in the U.S. state of Washington. The glacier is approximately in length, in width at its terminus and descends from . The glacier is separated by an arête from Boston Glacier to the east and south. Meltwaters from Forbidden Glacier flow into Moraine Lake.

Hanging Glacier is in North Cascades National Park in the U.S. state of Washington, on the north slopes of Mount Shuksan. Hanging Glacier is connected to Crystal Glacier at its uppermost margin, and also flows into Upper Curtis Glacier. Hanging Glacier is along the route taken in the first technical ascent of Mount Shuksan in 1939.

The Limmern Glacier () is a glacier situated in the Glarus Alps in the canton of Glarus in Switzerland. The glacier is situated below the mountains of Bifertenstock, to the south, and Schiben, to the north. Meltwater from the glacier flows eastwards into the Limmernsee and thence north into the Linth river. In 2005, the glacier had a length of .

The core of Ngozumpa glacier, and emerging Spillway lake The Ngozumpa glacier seen from the Ngozumpa Tse The Ngozumpa glacier, below the sixth highest mountain in the world Cho Oyu in Nepal, at , is the longest glacier in the Himalayas. Ngozumpa Glacier is a large persistent body of ice. It flows slowly due to stresses induced by its weight.

Vista Glacier is located on north slopes of Glacier Peak in the U.S. state of Washington. As is true with all the glaciers found on Glacier Peak, Vista Glacier is retreating. During the Little Ice Age, Vista Glacier extended down to an altitude of and was connected to Ermine Glacier to its east. From the end of the Little Ice Age to the mid-1950s, Vista Glacier experienced a general retreat upslope, followed by an advance during a cooler and wetter period until the mid-1970s.

No developed roads or paths lead to Penny Royal Glacier, though it is frequented by backcountry and wilderness enthusiasts. The glacier is most often accessed from the steep pass between Penny Royal Glacier and Bomber Glacier, from the valley floor at its terminus, or from the Backdoor Gap pass, which separates the glacier from Mint Valley. Penny Royal Glacier lies on the informal "Bomber Traverse" wilderness hiking route through the Talkeetna Mountains. Mountaineers may cross it en route to nearby peaks, and the glacier can be skied.

Ermine Glacier is located on north slopes of Glacier Peak in the U.S. state of Washington. As is true with all the glaciers found on Glacier Peak, Ermine Glacier is retreating. During the Little Ice Age, Ermine Glacier extended down to an altitude of and was connected to Vista Glacier to its west. From the end of the Little Ice Age to the mid-1950s, Ermine Glacier experienced a general retreat upslope, followed by an advance during a cooler and wetter period until the mid-1970s.

The Gorner Glacier () is a valley glacier found on the west side of the Monte Rosa massif close to Zermatt in the canton of Valais, Switzerland. It is about long (2014) and wide. The entire glacial area of the glacier related to Gorner Glacier is (1999), which makes it the second largest glacial system in the Alps after the Aletsch Glacier system; however it ranks only third in length behind the Aletsch and Fiescher Glacier, respectively. Numerous smaller glaciers connect with the Gorner Glacier.

Jackson Glacier is approximately the seventh largest of the remaining 25 glaciers in Glacier National Park located in the US state of Montana. A part of the largest grouping of glaciers in the park, Jackson Glacier rests on the north side of Mount Jackson. The glacier was most recently measured in 2005 at , yet when first documented in 1850, the glacier also included the now separate Blackfoot Glacier and together, they covered . Between 1966 and 2005, Jackson Glacier lost almost a third of its acreage.

Margerie Glacier had merged with this glacier in 1992. As the glacier started receding it got demerged from Margerie and only a small stream separates the two glaciers now.

Academy Glacier (), is a glacier in northwestern Greenland. Administratively it belongs to the Avannaata municipality. The glacier was named by Robert Peary after the Philadelphia Academy of Natural Sciences.

Wilma Glacier is the western of two glaciers entering the southern part of Edward VIII Ice Shelf in Kemp Land, East Antarctica. The second, eastern glacier is Robert Glacier.

San Francisco Glacier. The San Francisco Glacier is a glacier in Monumento Natural El Morado Natural Park a hundred kilometers away from Santiago, Chile. It is a tourist attraction.

Avsyuk Glacier () is a glacier on Arrowsmith Peninsula, Graham Land, flowing northwest to Shumskiy Cove.

Ranunculus glacialis, the glacier buttercup or glacier crowfoot, is a plant of the family Ranunculaceae.

Shani Glacier () is a glacier in the north of Shani Peak () in Naltar Valley, Pakistan.

Park Glacier is located on the northeast slopes of Mount Baker in the North Cascades of the U.S. state of Washington. Park Glacier descends to the Park Cliffs () along its eastern margin while the northern tongue of the glacier descends to nearly and is below Park Cliffs and Lava Divide. In the middle of its course, Park Glacier is connected to Rainbow Glacier to the north and Boulder Glacier to the south.

Errant Glacier () is a glacier, long, which lies on the east side of the Holyoake Range and drains south into Nimrod Glacier. This glacier offered a route to the southern party of the New Zealand Geological Survey Antarctic Expedition (1960–61) when they journeyed north from Nimrod Glacier in December 1960. It was named by them to describe the zigzag route of the party in traveling on the glacier in search for a route north.

Sem Kharak Glacier on the east, Deoban Glacier and Bankund Glacier on the south and Purbi Kamet Glacier on the north side of Bidhan Parbat. The River Dhauli Ganga emerges from Purbi Kamet Glacier and met Alaknanda River at Vishnu Prayag an 82 km journey from its mouth. Alaknanda river is one of the main tributaries of river Ganga. From Deoban and Bankund glacier emerges Amrit Ganga which after a short run joins Dhauli Ganga.

Boulder Glacier is located in the U.S. state of Montana in Glacier National Park (U.S.). The glacier is situated to the north of Boulder Peak and west of the Continental Divide. Between 1966 and 2005, Boulder Glacier lost more than 75 percent of its surface area. As of 2005 the glacier was measured to cover only , and no longer met the threshold often cited as the minimal area to qualify as an active glacier.

Smith Island Ritya Glacier (, ) is the steep 1.8 km long and 1.4 km wide glacier draining the southeast slopes of Imeon Range on Smith Island in the South Shetland Islands, Antarctica. It is situated northeast of Nosei Glacier, southeast of Kongur Glacier and south of Saparevo Glacier, flows southeastwards from Mount Christi and enters the head of Linevo Cove on Boyd Strait. The glacier is named after the settlement of Ritya in Northern Bulgaria.

Palilula Glacier (, ) is the 4 km long and 1.1 km wide steep valley glacier on Brabant Island in the Palmer Archipelago, Antarctica, situated south of Ralitsa Glacier, southwest of Paré Glacier and northwest of Gorichane Glacier. It drains the southwest slopes of Mount Rokitansky in Stribog Mountains, and flows south-southwestwards into Lanusse Bay east of Driencourt Point and northwest of Baykal Point. The glacier is named after the settlement of Palilula in Northwestern Bulgaria.

Harris Glacier is located in the US state of Montana in Glacier National Park. The glacier is situated in a cirque immediately to the northeast of Parke Peak at an elevation between and above sea level. The glacier covers an area of approximately and does not meet the threshold of often cited as being the minimum size to qualify as an active glacier. Between 1966 and 2005, the glacier lost 77 percent of its acreage.

Location of Oscar II Coast on Antarctic Peninsula. Dzhebel Glacier (, ) is the 15 km long and 11 km wide glacier on Oscar II Coast, Graham Land in Antarctica situated southwest of Jorum Glacier, northeast of Chuchuliga Glacier and southeast of Goodwin Glacier. It is draining from the slopes of Bruce Plateau and Forbidden Plateau, and flowing southeastwards to join Crane Glacier. The feature is named after the town of Dzhebel in southern Bulgaria.

Brenitsa Glacier (, ) is the 14 km long and 4.5 km wide glacier on Oscar II Coast, Graham Land in Antarctica situated southwest of Drygalski Glacier, west of Rogosh Glacier and east of Hektoria Glacier. Draining southwards from the south slopes of Foster Plateau east of Mount Quandary to flow into Vaughan Inlet, Weddell Sea next east of Hektoria Glacier. The feature is named after the settlements of Brenitsa in northern and northeastern Bulgaria.

With the joining of the termini on the north end of Crater Glacier in May 2008, the body of ice completely encircles the lava domes. Meltwater from the glacier gives rise to Loowit Creek. ;Pre-2004 eruption glacier caves of Crater Glacier New glaciers are forming on the crater wall, above and to the left of the lava dome (zoom in to view). In 2000, glacier caves were discovered on the then-smooth glacier surface.

Rhesus Glacier (, ) is a 7 km long and 2.5 km wide glacier draining the east slopes of the Trojan Range on Anvers Island in the Palmer Archipelago, Antarctica southeast of Paris Peak. Situated east of Iliad Glacier, south of Lipen Glacier and north of Thamyris Glacier. Flowing northeastwards into Fournier Bay south of Thompson Peninsula and north of Predel Point. The glacier is named after the King Rhesus of Thrace in Homer's Iliad.

Location of Fallières Coast on the Antarctic Peninsula. Marvodol Glacier (, ) is the 9.3 km long and 3.7 km wide glacier on Fallières Coast in Graham Land, Antarctica. It is situated south of Kashin Glacier, north of Forbes Glacier and east-southeast of Bucher Glacier, flows southwards between Shapkarev Buttress and Rudozem Heights, turns west at Stanhope Towers, and flows into Dogs Leg Fjord. The glacier is named after the settlement of Marvodol in Western Bulgaria.

Location of Fallières Coast on the Antarctic Peninsula. Kom Glacier (, ) is the 10 km long and 8 km wide glacier on the west side of Hemimont Plateau, Fallières Coast in Graham Land, Antarctica. It is situated south of Forbes Glacier and north of Swithinbank Glacier, drains westwards between Mercury Ridge and Zhefarovich Crag, and flows into Square Bay next north of Swithinbank Glacier. The glacier is named after Kom Peak in Western Balkan Mountains.

Hubbard Glacier is a glacier located in eastern Alaska and part of Yukon, Canada, and named after Gardiner Hubbard. Map of Hubbard Glacier Hubbard Glacier, Alaska, squeezes towards Gilbert Point on May 20, 2002. The glacier is close to sealing off Russell Fjord at top from Disenchantment Bay at bottom. The longest source for Hubbard Glacier originates from its snout and is located at about , approximately west of Mount Walsh with an elevation around .

The Siachen Glacier is a glacier located in the eastern Karakoram range in the Himalayas at about , just northeast of the point NJ9842 where the Line of Control between India and Pakistan ends. At long, it is the longest glacier in the Karakoram and second-longest in the world's non-polar areas.Siachen Glacier is long; Tajikistan's Fedchenko Glacier is long. The second longest in the Karakoram Mountains is the Biafo Glacier at .

Topographic map of Smith Island Gramada Glacier (, ) is a long glacier on Smith Island in the South Shetland Islands, Antarctica draining the southeast slopes of Imeon Range east of Riggs Peak, southeast of Madan Saddle and south of Neofit Peak. It is situated southwest of Armira Glacier and northeast of Letnitsa Glacier, and flows southeastward into Brashlyan Cove on Osmar Strait. The glacier is named after the town of Gramada in northwestern Bulgaria.Gramada Glacier.

Looking across the ice-margin Arctic Lake (currently drained) at the Tustemena Glacier The Tustumena Glacier is a glacier located on the Kenai Peninsula of Alaska. The Tustumena Glacier begins in the Harding Icefield and makes its way down west for about until its terminus roughly before Tustumena Lake. The glacier is retreating due to global warming. A small lake called Arctic Lake sits alongside Tustumena Glacier, with its outflow underneath the ice.

Roosevelt Glacier is located on the north slopes of Mount Baker in the North Cascades of the U.S. state of Washington. Roosevelt Glacier descends to nearly at Chromatic Moraine. In the middle of its course, Roosevelt Glacier is connected to Coleman Glacier to its south.

Ladder Creek Glacier is in North Cascades National Park in the U.S. state of Washington and is a northwest tongue of the larger Neve Glacier. Ladder Creek Glacier added between 1950 and 1979, but lost from 1979 to 2006. Ladder Creek Glacier descends from .

Darwin Glacier is a mountain glacier located on the north side of Mount Darwin in the Sierra Nevada, California. The glacier is located in Kings Canyon National Park. The glacier inherited its name from Mount Darwin, named for Charles Robert Darwin.Farquhar, Francis P. 1926.

Arikaree Glacier is an alpine glacier located in a cirque to the north of Arikaree Peak and south of Navajo Peak, in Roosevelt National Forest in the U.S. state of Colorado. The glacier is just east of the Continental Divide and south of Isabelle Glacier.

The 1850s is considered the Little Ice Age. Nisqually Glacier reached feet below the Glacier Bridge. On the west, Tahoma and South Tahoma Glaciers joined below Glacier Island along the Wonderland Trail. Emmons Glacier on the northeast reached within of the White River Campground.

Sprague Glacier is a small cirque glacier in Rocky Mountain National Park in the U.S. state of Colorado. Sprague Glacier is on the east side of the Continental Divide and southeast of Sprague Peak. Several small alpine lakes are near the foot of the glacier.

Rowe Glacier is an alpine glacier in Rocky Mountain National Park in the U.S. state of Colorado. It is north of Hagues Peak and the source of the North Fork Big Thompson River. Rowe Glacier was the first glacier to be identified in Colorado.

Lacroix Glacier () is a glacier between Suess Glacier and Matterhorn Glacier, which flows southeast into Taylor Valley in Victoria Land, Antarctica. It was mapped by the British Antarctic Expedition, 1910–13, under Robert Falcon Scott, and named after Alfred Lacroix, as was Mount Lacroix.

Lacuna Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins on the south side of Mount Foraker in the Alaska Range, moving southwest to join the Yentna Glacier, to which Lacuna is a tributary.

Stonebreen is a glacier located on the eastern coast of Edgeøya, Svalbard. Stonebreen is a glacier on Edgeøya, Svalbard. The glacier extends into the sea, and defines the eastern point of the island. Former names of the glacier include Disco Hook, Steinnase and Stansforelandshuk.

Mount Swanzy is a mountain summit located in Glacier National Park in the Selkirk Mountains of British Columbia, Canada. Mount Swanzy is surrounded by ice including the Bonney Glacier, Clarke Glacier, and Swanzy Glacier. Its nearest higher peak is Mount Bonney, to the west.

The Giétro Glacier or Giétroz Glacier () is a 4 km long valley glacier located in south-western Switzerland. The 1818 Giétro Glacier catastrophe, which led to lake outburst flood, is one of the most famous and most disastrous historical cases in the Swiss Alps.

Arensky Glacier () is an Antarctic glacier, lying east of Alyabiev Glacier and flows south from Beethoven Peninsula, Alexander Island, into the north end of Boccherini Inlet. The glacier was named by the USSR Academy of Sciences in 1987, after Anton Arensky, the Russian composer.

Flatbreen, Hornbreen, Storbreen Hornbreen ("Horn glacier") lies between Torell Land and Sørkapp Land on Spitsbergen, Svalbard. The glacier debouches into Hornsund. Former names of the glacier include Ramme Gletscher and Horn Glacier. Hornbreen has a length of about 15 km, and width of 8 km.

Kjenndalsbreen is a glacier in the municipality of Stryn in Vestland, Norway. The glacier is a side branch of the Jostedalsbreen glacier, and is included in the Jostedalsbreen National Park.

Athene Glacier () is a glacier, long, flowing east and merging with the terminus of Casey Glacier where it discharges into Casey Inlet, on the east coast of the Antarctic Peninsula.

Etonbreen is a glacier located on the west coast of Nordaustlandet, Svalbard. Etonbreen is a glacier on Nordaustlandet, Svalbard. The glacier debouches into Wahlenbergfjorden. It is named after Eton College.

Miar Glacier is a glacier that forms in the north of Miar Peak () in Hoper Valley in Nagar, Gilgit-Baltistan, Pakistan. It is a major component of the Barpu Glacier.

Johns Hopkins Glacier The Johns Hopkins Inlet is a stunning long fjord, which has several tide water glaciers. The Lamplugh Glacier is about away from the inlet and further inside is the Johns Hopkins Glacier, which is now the largest tidewater glacier in Glacier Bay and adjacent to it is the Gilman Glacier followed by the Hoonah Glacier further up. All these glaciers are tidewater glaciers. Ice blocks float in the inlet and it is quite hazardous for boating or kayaking; both activities have to be done with great caution.

The July 1 Glacier or Qiyi Glacier () is a glacier in Jiayuguan City, Gansu, China, and on the northern slope of the Tola Mountain in the Qilian Mountains. It is the closest glacier to cities in Asia, but it has been shrinking in recent years. This glacier was discovered by a geological worker of the Lanzhou Branch of the Chinese Academy of Sciences and a glacier scholar of the Soviet Union on July 1, 1958. The glacier is on a hillside with a slope that is less than 45 degrees.

Central and southern Sentinel Range map. Tulaczyk Glacier () is a steep valley glacier draining the west slope of Vinson Massif southwest of Príncipe de Asturias Peak, and descending between Cairns Glacier and Zapol Glacier in the Sentinel Range, Antarctica. The glacier flows southwestward and leaving the range, together with Cairns Glacier joins Nimitz Glacier west of Hodges Knoll and southeast of Klenova Peak. It was named by US-ACAN (2006) after Slawek M. Tulaczyk, Earth Sciences, University of California, Santa Cruz; USAP researcher of West Antarctic ice streams from 1998.

Location of Oscar II Coast on Antarctic Peninsula. Rogosh Glacier (, ) is the 29 km long and 5 km wide glacier on Oscar II Coast, Graham Land in Antarctica situated east of Brenitsa Glacier, south of Drygalski Glacier, and southwest of Zlokuchene Glacier and Risimina Glacier. Draining southwards from Kyustendil Ridge between Lovech Heights and Ivanili Heights, and turning eastwards north of Skilly Peak. At the ridge forming Cape Fairweather the glacier branches to flow into Artanes Bay to the south, and into Weddell Sea west of Pedersen Nunatak to the east.

Djerassi Glacier (, ) is a 2.8 km long and 1 km wide steep valley glacier situated south of Gorichane Glacier, west of the head of Malpighi Glacier, northwest of the head of Mackenzie Glacier, and north-northeast of Pirogov Glacier on Brabant Island in the Palmer Archipelago, Antarctica. It drains the west slopes of Harvey Heights and the north slopes of Mount Parry, and flows northwestwards into Lanusse Bay north of Venchan Peak. The glacier is named for the Bulgarian-American scientist Carl Djerassi (1923-2015), a co-inventor of the oral contraceptive pill.

The name Ferrar Glacier was originally applied both to the part of this glacier below its right turn and to the present Taylor Glacier. Thomas Griffith Taylor, geologist of the British Antarctic Expedition, 1910–13, under Scott, found evidence that these are not two parts of a single glacier but are two glaciers apposed. With this discovery Scott gave the names Ferrar Glacier and Taylor Glacier essentially as now applied; the Taylor Glacier makes a left turn at Cavendish Rocks and drains east along the north side of the Kukri Hills.

Lower Fremont Glacier is east of the Continental Divide in the northern Wind River Range in the U.S. state of Wyoming. The glacier is in the Fitzpatrick Wilderness of Shoshone National Forest, and is among the largest grouping of glaciers in the American Rocky Mountains. Lower Fremont Glacier flows to the southeast and the rapid retreat of this glacier has left behind lateral moraines and a proglacial lake. Lower Fremont Glacier is separated from the Bull Lake Glacier by a moraine and from the Upper Fremont Glacier by cliffs.

Topographic map of Smith Island. Chuprene Glacier (, ) is a long glacier draining the northwest slopes of Imeon Range on Smith Island in the South Shetland Islands, Antarctica. It is situated northeast of Bistra Glacier, southwest of Yablanitsa Glacier and northwest of Krivodol Glacier, Pashuk Glacier and Rupite Glacier, and flows southwest of Drinov Peak and Popovo Saddle, and west of Slatina Peak and Varshets Saddle southwestward along the northwest slopes of Antim Peak and Evlogi Peak into Drake Passage south of Villagra Point and north of Garmen Point. Bulgarian early mapping in 2009.

Nordenskiold Glacier (), is a large glacier in the Qaasuitsup Municipality, on the Western coast of Greenland.

Nordenskiold Glacier (), is a large glacier in the Avannaata Municipality, on the northwestern coast of Greenland.

Gildea Glacier in Craddock Massif, Antarctica is named after him.Gildea Glacier. Geographic Names Information System, USGS.

Foremost Terra Bus at Athabasca Glacier in the 1980s. A Terra Bus on the Athabasca Glacier.

The Geri-Freki Glacier, which descends north from Woden. is the only glacier in The Valhallas.

Dusty Glacier is heavily crevassed and the glacier ends in an ice fall at its terminus.

Tyndall Glacier or Geike Glacier is one of the largest glaciers in the Southern Patagonian Ice Field. It is located in the Torres del Paine National Park, Chile. The glacier has its main calving front in Geikie Lake and like its neighbor, Grey Glacier, it has been significantly retreating for the last years. The glacier is named after the Irish glaciologist John Tyndall.

Close view of Lamplugh Glacier. The Lamplugh Glacier was named by Lawrence Martin of the U.S. Geological Survey (USGS) around 1912 for the English geologist George William Lamplugh (1859–1926), who visited the Glacier Bay in 1884. The Glacier originates in the Brady Icefield to the east of Fairweather Range. The glacier has a width of about at the water face.

Sona Glacier is the Himalayan glacier situated in the eastern part of Uttarakhand in the Pithoragarh district of India.Sona Glacier is located at the base of five peaks of Panchchuli in the Lassar Yankti - Darma valley. With Meola glacier it forms the famous Panchchuli glacier as mixed glacial system. One can reach here as glacial trek through Tawaghat-Bailing-Son--Duktu-.

Harbour Glacier () is a glacier flowing north from Wilson Piedmont Glacier into Granite Harbour east of the Couloir Cliffs, Victoria Land, Antarctica, where it forms the Harbour Glacier Tongue. It was named by the Advisory Committee on Antarctic Names in 2005, in association with "Harbour Ice Tongue" (now Harbour Glacier Tongue), which was named by the British Antarctic Expedition, 1910–13.

Repeater Glacier () is a steep glacier, long, flowing east from Ponder Peak in the Asgard Range of Victoria Land. This glacier and the Commanda Glacier, close southward, drain the eastern slopes of the Mount Newall massif before entering lower Newall Glacier. Named by the New Zealand Geographic Board in 1998 in recognition of the radio repeater installed by New Zealand on Mount Newall.

Baudissin Glacier () is a tidewater glacier on the north side of Heard Island. in the southern Indian Ocean. Located 1 nautical mile (1.9 km) west of Challenger Glacier, Baudissin Glacier is 1.5 nautical miles (2.8 km) wide and flows into the western part of Corinthian Bay. The terminus of Baudissin Glacier is located at the western side of Corinthian Bay, at Sealers Cove.

Bary Glacier () is a glacier flowing west into Jacobsen Bight, South Georgia, south of Christophersen Glacier. The glacier cuts through the longest sedimentary sequence on the island, from Christophersen Glacier to Cape Darnley. It was named by the UK Antarctic Place-Names Committee in 1982 after Thomas de Bary, one of the first directors of the Compañía Argentina de Pesca from 1904.

Yentna Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Alaska Range between Mount Russell and Mount Foraker, moving southwest. It is the source of the east fork of the Yentna River. Lacuna Glacier is a major tributary, and Dall Glacier enters the glacial valley just below Yentna Glacier's present terminus.

Shadows Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Kichatna Mountains on the north side of the Cathedral Spires, moving north. It receives neighboring Shelf Glacier as a tributary, and together with Cul-de-sac Glacier feeds the west fork of the Yentna River.

The largest retreat was on O'Higgins Glacier, which during the period 1896–1995 retreated . The Perito Moreno Glacier is long and is a major outflow glacier of the Patagonian ice sheet, as well as the most visited glacier in Patagonia. Perito Moreno Glacier is in equilibrium, but has undergone frequent oscillations in the period 1947–96, with a net gain of .

Giridava Glacier (, ) is long and wide glacier on the west side of Urda Ridge on Clarence Island in the South Shetland Islands, Antarctica situated north of Skaplizo Glacier and southwest of Bersame Glacier. It drains the slopes of Mount Irving, flows northwestwards and enters Chinstrap Cove east of Vaglen Point. The glacier is named after the Thracian settlement of Giridava in Northern Bulgaria.

Blue Glacier is a large glacier located to the north of Mount Olympus in the Olympic Mountains of Washington. The glacier covers an area of and contains of ice and snow in spite of its low terminus elevation. The glacier length has decreased from about in 1800 to in the year 2000. Just in the period from 1995 and 2006, Blue Glacier retreated .

Topographic map of Smith Island. Yablanitsa Glacier (, ) is a 1.8 km long glacier on Smith Island in the South Shetland Islands, Antarctica. It is situated north-northeast of Chuprene Glacier, southwest of Vetrino Glacier and northwest of Ovech Glacier, and flows west of Drinov Peak into Cabut Cove. The feature is named after the town of Yablanitsa in northern Bulgaria.

Topographic map of Smith Island. Rupite Glacier (, ; ) is a long glacier on Smith Island, South Shetland Islands draining the southeast slopes of Imeon Range east of the summit Mount Foster and southeast of Evlogi Peak. It is situated southeast of Chuprene Glacier, southwest of Pashuk Glacier and northeast of Landreth Glacier, and flows southeastward into Osmar Strait. Bulgarian early mapping in 2008.

Utstikkar Glacier () is a broad glacier flowing north from the vicinity of Moyes Peak in Antarctica and terminating in Utstikkar Glacier Tongue between Utstikkar Bay to the east and Allison Bay to the west. The glacier was mapped and named Utstikkarbreen (the out-jutting glacier) by Norwegian cartographers working from aerial photographs taken by the Lars Christensen Expedition in January–February 1937.

Meltwater from Mount Rainier's Edmunds Glacier, South Mowich Glacier, and North Mowich Glacier feed the north and south branches of the Mowich River. Other rivers originate in glaciers just south and north of the Mowich River's glaciers. To the south, the Puyallup Glacier gives rise to the Puyallup River, while to the north the Carbon Glacier creates the Carbon River.

NASA Radarsat Image of the Beardmore Glacier in Antarctica Showing Glacier Names Berwick Glacier () is a tributary glacier, long, flowing southeast between the Marshall Mountains and the Adams Mountains to enter Beardmore Glacier at Willey Point in Antarctica. It was named by the British Antarctic Expedition, 1907–09, (BrAE) after HMS Berwick, a vessel on which Lieutenant Jameson B. Adams of the BrAE had served. The map of the British Antarctic Expedition, 1910–13, and some subsequent maps transpose the positions of Berwick Glacier and Swinford Glacier. The latter lies southwestward, and the original 1907–09 application of Berwick Glacier is the one recommended.

Biafo Glacier in Gilgit Baltistan Biafo Glacier Biafo Glacier The Biafo Glacier () is a long glacier in the Karakoram Mountains of Gilgit Baltistan, Pakistan, which meets the long Hispar Glacier at an altitude of at Hispar La (Pass) to create the world's longest glacial system outside the polar regions. This highway of ice connects two ancient mountain kingdoms, Nagar, in the west with Baltistan in the east. The traverse uses 51 of the Biafo Glacier's 67 km and all of the Hispar Glacier to form a glacial route. The Biafo Glacier presents a trekker with several days of strenuous boulder hopping, with views throughout and Snow Lake near the high point.

Snow Lake, consisting of parts of the upper Biafo Glacier and its tributary glacier Sim Gang, is one of the world's largest basins of snow or ice in the world outside the polar regions, up to in depth. The Biafo Glacier is the world's third longest glacier outside the polar regions, second only to the Siachen Glacier, India-Pakistan and Tajikistan's long Fedchenko Glacier. Campsites along the Biafo are located off of the glacier, adjacent to the lateral moraines and steep mountainsides. The first three (heading up from the last village before the glacier, the thousand-year-old Askole village) are beautiful sites with flowing water nearby.

Concordia K2 Trek The glacier gives rise to the Braldo River which is a tributary of Shigar River, which is a tributary of the Indus River. Several large tributary glaciers feed the main Baltoro Glacier, including the Godwin Austen Glacier, flowing south from K2; the Abruzzi and the various Gasherbrum Glaciers, flowing from the Gasherbrum group of peaks; the Vigne Glacier, flowing from Chogolisa, and the Yermandendu Glacier, flowing from Masherbrum. The confluence of the main Baltoro Glacier with the Godwin Austen Glacier is known as Concordia; this location and K2 base camp are popular trekking destinations. The trough of this glacier is very wide.

The Banski Suhodol Glacier in July 2012 The Banski Suhodol Glacier (, Lednika v Banski Suhodol) is a small glacier (glacieret) in the Pirin Mountains of Bulgaria. It lies below the Kutelo peak (2908 m.) in the upper Banski Suhodol Valley (). The glacier is on the northern slope of the Kutelo summit and is shaded from the east by the Koncheto ridge. After the nearby Snezhnika glacier (latitude of 41°46′09″ N) Banski Suhodol glacier is the southernmost in Europe, followed by three small glaciers below the Maja Jezerce summit in northern Albania, the Calderone glacier in the Gran Sasso mountain in Italy, and Debeli Namet glacier in Montenegro.

Humboldt Glacier () is one of the major glaciers in northern Greenland. The glacier is named after German naturalist Alexander von Humboldt and is the widest tidewater glacier in the Northern Hemisphere.

Kvitbreen (White Glacier) is a glacier in Ny-Friesland at Spitsbergen, Svalbard. It located south of Newtontoppen, and is connected with the glacier of Veteranen at the other side of Trebrepasset.

Alberts Glacier () is a heavily crevassed glacier in Antarctica. It is about long, and flows east from Avery Plateau, Graham Land, until entering Mill Inlet between Balch Glacier and Southard Promontory.

Uvêrsbreen (Bad Weather Glacier) is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of about 25 kilometers. The glacier debouches into Engelskbukta, after merging with Comfortlessbreen.

Rink Glacier (), is a glacier in NW Greenland. Administratively it belongs to the Avannaata municipality. This glacier was named after Danish geologist and explorer of Greenland Hinrich Johannes Rink (1819 - 1893).

Whatcom Glacier is in North Cascades National Park in the U.S. state of Washington, in a cirque to the northeast of Whatcom Peak. Whatcom Glacier is approximately north of Challenger Glacier.

The glacier lies entirely within Mount Hood Wilderness. Between 1907 and 2004, Reid Glacier lost 35% of its surface area. The glacier terminus has retreated by over the same time period.

Hakebreen ("The Hook Glacier") is a glacier in Haakon VII Land at Spitsbergen, Svalbard. It has a length of about five kilometers, and is a tributary glacier to the Fjortende Julibreen. The glacier is surrounded by the mountains of Målarryggen, Foreltinden, Forelryggen, Giardtinden, Fregatten and Haken.

Wolf Glacier is in the U.S. state of Montana. The glacier is situated in the Beartooth Mountains at an elevation of in a north facing cirque to the east of Wolf Mountain. The glacier covers approximately and several small proglacial lakes are near the glacier terminus.

Waldo Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range on the south-southeast slopes of Mount Jefferson. Starting near an elevation of , the glacier extends down to . The glacier is named after John B. Waldo, as is Waldo Lake.

The Lauteraar Rothörner are a multi-summited mountain of the Bernese Alps, overlooking the Unteraar Glacier in the canton of Bern. They lie one kilometre south-east of the Hugihorn, on the range separating the Strahlegg Glacier from the Lauteraar Glacier, both tributaries of the Unteraar Glacier.

Bagrote, Hunza, Nagar and Hispar Glacier Hispar Glacier () is a long glacier in the Karakoram Mountains of Gilgit–Baltistan, Pakistan which meets the long Biafo Glacier at the Hispar La (Pass) at an altitude of to create the world's longest glacial system outside of the polar regions.

Straightaway Glacier, also known as Crosson Glacier, is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Alaska Range on the north side of Mount Crosson, moving northwest. It is a source of the Foraker River.

Jeffery Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Alaska Range on the north side of Denali directly below the Wickersham Wall, heading northeast to join Peters Glacier after the latter's Tluna Icefall.

Rupal Glacier or Tashain Glacier is a glacier in the Great Himalaya subrange of Himalayas. It starts north of an unnamed peak () and flows northeastward, north of Laila Peak (Rupal Valley) and south of Nanga Parbat's many peaks. The meltwater from the glacier forms Rupal River.

When the whole glacier is considered, it is the largest glacier in Sweden. The glacier's highest point is above sea level and its lowest point is at an elevation of . The glacier has retreated in recent years. The lake Låmivatnet lies just south of the glacier.

Ascent Glacier () is a glacier, wide, flowing north to enter Argosy Glacier in the Miller Range just east of Milan Ridge. It was named by the New Zealand Geological Survey Antarctic Expedition (1961–62) who used this glacier to gain access to the central Miller Range.

Reid Glacier is an alpine glacier located on the west slope of Mount Hood in the U.S. state of Oregon. It ranges in elevation from about . The glacier is the source of the Sandy River. The upper extent of the glacier is known for extensive crevasses.

Fox Glacier School Fox Glacier School is the sole school in Fox Glacier, serving approximately students from Years 1 to 8 (ages 5 to 12). The school was established in 1877. The nearest secondary school to Fox Glacier is South Westland Area School, away in Hari Hari.

Lobby of Glacier Park Lodge Glacier Park Lodge is located just outside the boundaries of Glacier National Park in the village of East Glacier Park, Montana, United States. The lodge was built in 1913 by the Glacier Park Company, a subsidiary of the Great Northern Railway. It was the first of a series of hotels built in and near Glacier National Park by the Great Northern to house visitors brought to the park by the railroad.

Montigny Glacier () is a steep tributary glacier in the Bowers Mountains of Antarctica, flowing eastward and at the terminus coalescing with Irwin Glacier (from the south), with which it enters the larger Graveson Glacier. Montigny Glacier was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for glaciologist Raymond J. Montigny, who participated in the study of Meserve Glacier in 1966–67.

Amalia Glacier, also known as Skua Glacier, is a tidewater glacier located in Bernardo O'Higgins National Park on the edge of the Sarmiento Channel. The glacier originates in the Southern Patagonian Ice Field. From 1945 to 1986, its terminus retreated , being, along with the recession of the O'Higgins Glacier, the most dramatic retreat of the glaciers of the mentioned icefield during that period. The glacier partially surrounds Reclus volcano and erodes the northern flank of it.

Miche Wabun Glacier is a glacier remnant (glacieret) in the U.S. state of Montana in the northeastern region of Glacier National Park. The glacieret is situated in a cirque to the east of Goat Haunt Mountain. Miche Wabun Glacier was measured in 2010 to have retreated to less than in area, considered to be a minimal size to qualify as being considered an active glacier. Between 1966 and 2005, the glacier lost over 55 percent of its surface area.

Agassiz Glacier is in Glacier National Park in the U.S. state of Montana. It is named after Louis Agassiz, a Swiss-American glaciologist. The glacier is situated in a cirque to the southeast of Kintla Peak west of the Continental Divide. Agassiz Glacier is one of several glaciers that have been selected for monitoring by the U.S. Geological Survey's Glacier Monitoring Research program, which is researching changes to the mass balance of glaciers in and surrounding Glacier National Park.

Map of Union Glacier. Union Glacier Union Glacier (), is a large, heavily crevassed glacier which receives the flow of several tributaries and drains through the middle of the Heritage Range, Ellsworth Mountains, Antarctica. The glacier drains from the plateau at Edson Hills on the west side of the range and flows east between Pioneer Heights and Enterprise Hills. Union Glacier was mapped by U.S. Geological Survey (USGS) from surveys and U.S. Navy (USN) air photos, 1961–66.

Ipasha Glacier is located in the US state of Montana in Glacier National Park. The glacier is situated in a cirque to the southeast of Chaney Glacier and immediately east of the Continental Divide at an elevation between and above sea level. The glacier covers an area of approximately as measured in 2005, which is a third smaller than it was in 1966. Melt water from the glacier flows over Ipasha Falls en route to Ipasha Lake.

Location of Oscar II Coast on Antarctic Peninsula. Stob Glacier (, ) is the 16 km long and 13 km wide glacier on Oscar II Coast, Graham Land in Antarctica situated southwest of Chuchuliga Glacier, east-southeast of Somers Glacier and south-southeast of Talbot Glacier. It is draining from the slopes of Bruce Plateau north of Bersin Ridge, and flowing eastwards to join Crane Glacier. The feature is named after the settlement of Stob in western Bulgaria.

Compton Glacier is a glacier, long, flowing northeast from the lower slopes of the Big Ben massif to the northeast side of Heard Island in the southern Indian Ocean. Its terminus is located at Compton Lagoon, between Gilchrist Beach and Fairchild Beach. To the northwest of Compton Glacier is Ealey Glacier, whose terminus is located close southeast of Cape Bidlingmaier. To the southeast of Compton Glacier is Brown Glacier, whose terminus is located at Brown Lagoon.

Downes Glacier () is a broad tidewater glacier on the north side of Heard Island in the southern Indian Ocean. It flows north on both sides of Cape Bidlingmaier to the north coast of Heard Island. To the east of Downes Glacier is Ealey Glacier, whose terminus is located close southeast of Cape Bidlingmaier. To the west of Downes Glacier is Challenger Glacier, whose terminus is located at the eastern side of Corinthian Bay, close west to Saddle Point.

Gotley Glacier is a well-defined glacier, long, descending from the ice- covered slopes of the Big Ben massif to the southwest side of Heard Island in the southern Indian Ocean. Its terminus is located between Cape Arkona and Cape Labuan. To the east of Gotley Glacier is Deacock Glacier, whose terminus is located between Cape Labuan and Long Beach. To the northwest of Gotley Glacier is Lied Glacier, whose terminus is located between Cape Arkona and Cape Pillar.

Abbotsmith Glacier () is a well-defined glacier, long, descending from the ice-covered west slopes of Big Ben to the west side of Heard Island in the southern Indian Ocean. The glacier lies between Walsh and Henderson Bluffs. Surveyed in 1948 by the ANARE (Australian National Antarctic Research Expeditions) who named it for John Abbotsmith, engineer with the party. To the south of Abbotsmith Glacier is Lied Glacier, while Allison Glacier is immediately to the north.

Sentinel Range map. Drama Glacier (, ) is the 10 km long and 1.5 km wide glacier on the east side of southern Sentinel Range in Ellsworth Mountains, Antarctica, which is situated north of Carey Glacier and Gabare Glacier, east of the east-northeast ridge of Mount Landolt, and south of Razboyna Glacier. It is draining east-northeastwards to join Rutford Ice Stream northeast of Long Peak. The glacier is named after the settlement of Drama in Southeastern Bulgaria.

Fjallsárlón is a glacier lake at the south end of the Icelandic glacier Vatnajökull. Fjallsjökull which is part of the bigger glacier reaches down to the water of the lake and some ice-bergs are drifting by on its surface. The glacier calving into the lagoon is a part of Vatnajökull National Park and the better known glacier lake Jökulsárlón is not far from there. From the glacier lake Breiðárlón a little river flows into the Fjallsárlón.

Map of Sentinel Range. Marsa Glacier (, ) is the 5 km long and 1.5 km wide glacier in Bangey Heights on the east side of the main ridge of north-central Sentinel Range in Ellsworth Mountains, Antarctica. It is situated northeast of Patleyna Glacier and northwest of the head of Padala Glacier. The glacier drains the north slopes of Golemani Peak, flows north-northwestwards between Oreshak Peak and Fucha Peak, and joins Embree Glacier west of Mount Schmid.

Map of northern Sentinel Range. Vidul Glacier (, ) is the 7.5 km long and 1.4 km wide glacier on the east side of the main crest of northern Sentinel Range in Ellsworth Mountains, Antarctica. It is situated northwest of Skaklya Glacier and southwest of the middle course of Newcomer Glacier. The glacier drains the north slopes of Mount Reimer and the east slopes of Mount Dawson, flows northwards and joins Newcomer Glacier west of Mount Warren in Gromshin Heights.

East Nooksack Glacier is in North Cascades National Park in the U.S. state of Washington, on the eastern slopes of Mount Shuksan. East Nooksack Glacier is only , but fills the upper portions of the Nooksack Cirque, spanning more than . East Nooksack Glacier is connected to Crystal Glacier at its uppermost section at . East Nooksack Glacier extends from Nooksack Tower to the northwest to Seahpo Peak to the southeast and meltwater from the glacier flows into the Nooksack River.

At the maximum extended position the glacier is once again sensitive to changing climate. Brady Glacier and Baird Glacier are examples of glaciers currently at this point. Brady Glacier has been thinning during the last two decades due to the higher equilibrium line altitudes accompanying warmer conditions in the region, and its secondary termini have begun to retreat. A glacier can remain at this position for sometime, a century at least in the case of Brady Glacier.

William Glacier () is a glacier flowing south from the interior highlands of Anvers Island to the head of Börgen Bay on the southeast coast of the island, in the Palmer Archipelago. Discovered by the Belgian Antarctic Expedition, 1897–99, under Gerlache, and charted by them simply as a "grand glacier." The name William Glacier first appears on a chart based upon a 1927 survey by DI personnel on the Discovery. Gateway Ridge separates William Glacier from Hooper Glacier.

South Cascade Glacier is a large alpine glacier in the North Cascades of Washington, USA. It is bordered on the east by Sentinel Peak, and is about north of Glacier Peak in the Glacier Peak Wilderness. Meltwater from the glacier flows directly into South Cascade Lake, which feeds the South Fork Cascade River, which is a tributary of the Skagit River. The South Cascade Glacier has been closely monitored by glaciologists studying the effects of climate on glaciers.

Location of Nordenskjöld Coast. Mundraga Bay (, ) is the 28.6 km wide bay indenting for 23 km Nordenskjöld Coast in Graham Land, Antarctica. It is entered east of Fothergill Point and west of Cape Sobral. Local coastline is modified as a result of the Larsen A Ice Shelf disintegration and the subsequent retreat of the inflowing Darvari Glacier, Boryana Glacier, Desudava Glacier, Dinsmoor Glacier, Bombardier Glacier and Edgeworth Glacier in the 1990s and the early 21st century.

A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land, and then melts, filling the depression created by the glacier.

Hydrografbreen ("The Hydrographer Glacier") is a glacier in Oscar II Land at Spitsbergen, Svalbard. The glacier has a length about eight kilometers, and extends from the mountain range of Holmesletfjella to Jørgenfjellet.

Russell Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range on the northwest slopes of Mount Jefferson. Russell Glacier is situated at an elevation between .

Overcoat Glacier is in the U.S. state of Washington. Overcoat Glacier is in both Wenatchee and Snoqualmie National Forests and flows north from Overcoat Peak and Chimney Rock. Overcoat Glacier descends from .

Steenstrup Glacier (), is a glacier in NW Greenland. Administratively it belongs to the Avannaata municipality. This glacier was named after Danish geologist and explorer of Greenland K. J. V. Steenstrup (1842 - 1913).

The Trift Glacier () is a long glacier (2005) in the Urner Alps near Gadmen, in the extreme east of the canton Berne in Switzerland. Trift Glacier viewing south in winter of 2014.

The National Park Service is currently studying Noisy Creek Glacier as part of their glacier monitoring project.

Hayes Glacier is a tidewater glacier in the Avannaata municipality, located on the northwestern shore of Greenland.

He is commemorated in the naming of the Mill Glacier, a branch of the Beardmore Glacier at .

Sif Glacier (), is a glacier in northern Greenland. Administratively it belongs to the Northeast Greenland National Park.

King Oscar Glacier () is a large glacier in the Avannaata Municipality, on the northwestern coast of Greenland.

The Wenden Glacier () is a glacier in the Urner Alps in the canton of Berne in Switzerland.

Goodspeed Glacier () is a small hanging glacier on the south wall of Wright Valley in Victoria Land, Antarctica, between Hart Glacier and Denton Glacier. It was named by U.S. geologist Robert Nichols after Robert Goodspeed, geological assistant to Nichols at nearby Marble Point in the 1959–60 field season.

Hart Glacier is a small hanging glacier on the south wall of Wright Valley, Victoria Land, Antarctica, between Meserve Glacier and Goodspeed Glacier. It was named by U.S. geologist Robert Nichols for Roger Hart, a geological assistant to Nichols at nearby Marble Point in the 1959–60 field season.

Astronaut Glacier () is a broad glacier, tributary to upper Aviator Glacier, flowing south-west and joining the latter just west of Parasite Cone in Victoria Land. It was named by the northern party of the New Zealand Geological Survey Antarctic Expedition, 1962-63, in association with nearby Aeronaut Glacier.

Whitewater Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range on the east and northeast slopes of Mount Jefferson. Starting near the summit at an elevation over , the glacier extends down to . From north to south, the glacier is nearly wide.

Many Glacier Hotel The List of Glacier National Park (U.S.) references identifies English language historic, scientific, ecological, cultural, tourism, social, and advocacy books, journals and studies on the subject of Glacier National Park (U.S.) topics published since 1870 and documented in Glacier related bibliographies and other related references.

Coe Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range on the north slope of Mount Hood, at an elevation between . Between 1907 and 2004, Coe Glacier lost 15% of its surface area. The glacier terminus retreated over the same time period.

Understanding glacier environmental changes requires many techniques and perspectives. Precise measurements from sensors on satellites and airplanes quantify ongoing glacier volume changes; landforms and lake sediments reveal past glacier-climate changes; the hydrochemistry of surface waters reflects glacier melt contribution; and computer simulations help explain past and future dynamics.

Hedgehogfonna is a glacier field in Sørkapp Land at Spitsbergen, Svalbard. It is located west of the mountain of Hedgehogfjellet, and is separated from the glacier of Vasil'evbreen by Skilfonna. The glacier of Sykorabreen extends seven kilometers northwards from Hedgehogfonna, and the glacier of Tromsøbreen extends six kilometers southwards.

Breiðárlón is a glacier lake at the south end of the Icelandic glacier Vatnajökull. The glacier calving into the lagoon is a part of Vatnajökull National Park and the better known glacier lake Jökulsárlón is not far from there. From Breiðárlón a little river flows into the Fjallsárlón.

Pastra Glacier (, ) is a 4.8 km long and 2 km wide glacier in the central part of Trinity Island in the Palmer Archipelago, Antarctica. Draining northwards to flow into Milburn Bay. The glacier is named after the settlement of Pastra in western Bulgaria.SCAR Composite Gazetteer of Antarctica: Pastra Glacier.

Matanuska Glacier is a valley glacier in the US state of Alaska. At long by wide, it is the largest glacier accessible by car in the United States. Its terminus feeds the Matanuska River.Matanuska River It lies near the Glenn Highway about north-east of Anchorage in Glacier View.

Namik Glacier is situated in the Pithoragarh district of Uttarakhand state in India. The glacier is situated on the Kumaon Himalayas at an altitude of . This glacier is the source of the Ramganga River. The glacier is surrounded by the following peaks: Nanda Devi , Nanda Kot , and Trishuli .

Haselton Glacier () is a glacier flowing east-northeast between Gibson Spur and the Apocalypse Peaks, terminating as a hanging glacier at Barwick Valley in Victoria Land. Named in 2005 by the Advisory Committee on Antarctic Names in association with Haselton Icefall, a heavily crevassed upper part of the glacier.

Trient Glacier The Trient Glacier () is a 4.3 km long glacier (2007) situated in the Mont Blanc Massif in the canton of Valais in Switzerland. In 1973 it had an area of 6.4 km². The upper part of the glacier forms a large plateau named Plateau du Trient.

Matusevich Glacier is a broad glacier about long, with a well developed glacier tongue, flowing to the coast of East Antarctica between the Lazarev Mountains and the northwestern extremity of the Wilson Hills.

Attlee Glacier () is a glacier long, which flows east-southeast from the plateau escarpment on the east side of Graham Land to the head of Cabinet Inlet to the north of Bevin Glacier.

Area map of Skelton glacier. Skelton Glacier is a large glacier flowing from the polar plateau into the Ross Ice Shelf at Skelton Inlet on the Hillary Coast, south of Victoria Land, Antarctica.

Damma Glacier The Damma Glacier () is a 2 km long glacier (2005) situated in the Urner Alps in the canton of Uri in Switzerland. In 1973 it had an area of 5.09 km².

Rabotbreen is a glacier in Sabine Land at Spitsbergen, Svalbard. The glacier is a tributary glacier to Fimbulisen, and is located in the upper part of Sassendalen. Nearby mountains are Bairdfjellet and Moskusryggen.

Fountain Glacier () is a glacier between Nylen Glacier and Catspaw Glacier in the Asgard Range, McMurdo Dry Valleys, Antarctica. It flows south into Pearse Valley. It was named by the Advisory Committee on Antarctic Names (2004) after Andrew G. Fountain of the Department of Geology, Portland State University, a United States Antarctic Program investigator in glacier mass balance studies of the McMurdo Dry Valleys, 1993–2003.

They are bounded by Patleyna Glacier to the west, Embree Glacier to the northwest and northeast, and Kopsis Glacier to the southeast, and linked to Probuda Ridge to the southwest by Chepino Saddle, and to Maglenik Heights to the south by Panicheri Gap. Their interior is drained by Marsa Glacier and Padala Glacier. The heights are named after the settlement of Bangeytsi in northern Bulgaria.

It is surrounded by Glaciers on both the side Uttari Rishi Glacier, on the southern side and Bagini Glacier on the northern side. The River from Bagini Glacier met with Dhauli Ganga at Jumma. Changabang Bamak (Glacier) and Uttari Rishi Bamak (Glacier) also met Dhauli Ganga through Rishi Ganga gorge. later Dhauli Ganga met with Alaknanda river at Vishnu Prayag two main tributaries of Ganga.

Nandakhani stands between Shalang Glacier on the eastern side and Pindari Glacier on the western side. On the southern side guards the Kafni Glacier. Shalang glacier flows from south-west to south-east and joins Goriganga River that later joins the Kali River at Jauljibi. On the southern side from Kafni glacier emerges Kafni river and after a short run it joins Pindari river at Dwali.

Nanda Bhanar stands between Shalang Glacier on the eastern side and Pindari Glacier on the western side. On the southern side guards the Kafni Glacier. Shalang glacier flows from south-west to south-east and joins Goriganga River that later joins the Kali River at Jauljibi. On the southern side from Kafni glacier emerges Kafni river and after a short run it joins Pindari river at Dwali.

Longs Peak has one remaining glacier named Mills Glacier. The glacier is located around 12,800 feet (3,900 m)TopoQuest - Mills Glacier, USGS Longs Peak (CO) Topo Map at the base of the Eastern Face, just above Chasm Lake. A permanent snowfield, called The Dove, is located north of Longs Peak. Longs Peak is one of fewer than 50 mountains in Colorado that have a glacier.

Squak Glacier is located on the southeast slopes of Mount Baker in the North Cascades of the U.S. state of Washington. Squak Glacier is connected to Easton Glacier to the east and Talum Glaciers to the west. Between 1850 and 1950, Squak Glacier retreated . During a cooler and wetter period from 1950 to 1979, the glacier advanced but between 1980 and 2006 retreated back .

Sentinel Range map. Gabare Glacier (, ) is the long and wide glacier in Petvar Heights on the southeast side of Sentinel Range in Ellsworth Mountains, Antarctica situated northwest of Divdyadovo Glacier, northeast of the head of Carey Glacier, and southeast of Drama Glacier. It is flowing eastwards to leave the range east-southeast of Long Peak. The feature is named after the settlement of Gabare in northwestern Bulgaria.

As of recently, there has been a re-establishment of glacier monitoring sites in Kyrgyzstan with the Abramov glacier, Golubin glacier, Batysh Sook glacier, and Glacier No. 345. Observations and research over the last five decades show that, overall, the Central Asian glaciers portray more mass loss than mass gain. From 2000 to 2100, glacial areas are expected to be reduced between 64 and 95 percent.

This glacier is located in the far northwest of Greenland, to the north of the Thule Air Base. It is one of four large glaciers which feeds the Wolstenholme Fjord (sometimes referred to as "the world's largest ice machine"). The other glaciers are the Chamberlin Glacier, the Knud Rasmussen Glacier, and the Harald Moltke Glacier. The Salisbury Glacier is over in length and is approximately in width.

Isabelle Glacier is an alpine glacier located southwest of Shoshoni Peak, in Roosevelt National Forest in the US state of Colorado. The glacier is immediately east of the Continental Divide on the opposite side of the divide from Fair Glacier. Isabelle Glacier is the source of the South Saint Vrain Creek and can be reach by trail and is a round-trip hike from the trailhead.

Dome Glacier is in Snoqualmie National Forest in the U.S. state of Washington and is on the north slopes of Dome Peak. Dome Glacier flows generally west for a distance of approximately , maintaining a generally shallow gradient between at which point it descends in a large icefall to approximately . An arête separates the glacier from Dana Glacier to the northwest and Chickamin Glacier to the east.

Podayva Glacier (, ) is the 4.5 km long and 3 km wide glacier on Pasteur Peninsula, Brabant Island in the Palmer Archipelago, Antarctica, situated northeast of Dodelen Glacier and west of Burevestnik Glacier. It drains the north slopes of Stribog Mountains, flows northwards and enters the sea east of Cape Roux and west of Marinka Point. The glacier is named after the settlement of Podayva in Northeastern Bulgaria.

Ptarmigan Glacier is located on north slopes of Glacier Peak in the U.S. state of Washington. As is true with all the glaciers found on Glacier Peak, Ptarmigan Glacier is retreating. During the Little Ice Age, Ptarmigan Glacier extended down to an altitude of but aside from a small advance during the 1970s, has retreated significantly since the end of the Little Ice Age.

Sphinx Glacier is in the Wind River Range, Bridger-Teton National Forest, in the U.S. state of Wyoming. The glacier is situated on the southern slope of Mount Woodrow Wilson () and immediately west of the Continental Divide. The glacier is flanked on the east by a mountain known as The Sphinx (). Sphinx Glacier is on the opposite side of the Continental Divide from Dinwoody Glacier.

Green Lake Glacier is in North Cascades National Park in the U.S. state of Washington and is immediately northeast of Bacon Peak. Green Lake Glacier descends from a ridge extending from the east of Bacon Peak. The glacier forms two tongues descending to the north of the ridge from . The ridge is an arête which separates Green Lake Glacier from Diobsud Creek Glacier to the south.

Mertz Glacier Mertz Glacier () is a heavily crevassed glacier in George V Coast of East Antarctica. It is the source of a glacial prominence that historically has extended northward into the Southern Ocean, the Mertz Glacial Tongue. It is named in honor of the Swiss explorer Xavier Mertz. The Mertz- Ninnis Valley () is an undersea valley named in association with the Mertz Glacier and the Ninnis Glacier.

Hourihan Glacier () is a glacier draining the south slopes of Ward Tower in the Britannia Range, Antarctica, and flowing southeast to Merrick Glacier. It was named by the Advisory Committee on Antarctic Names in association with Byrd Glacier and Merrick Glacier, after Captain Joseph J. Hourihan, U.S. Navy, captain of , a cargo vessel of U.S. Navy Operation Highjump, 1946–47, led by Admiral Byrd.

Formerly known as the Great Glacier, it was a major tourist attraction during the Glacier House period from 1886 to 1925. The glacier's terminus, formerly a short walk from the Glacier House site, has retreated far up the mountainside. The névé of the glacier spreads far to the south, also spawning the Geikie Glacier. Most of the large glacial features are south of the Trans-Canada corridor.

Osmaston surveyed the Sanctuary's northern glacier while Shipton explored the Changabang glacier. While Osmaston turned to the southern glacier, Shipton descended the Rishi Ganga gorge, made a failed attempt on Dunagiri, crossed the Bagini Pass and descended the Bagini glacier to the north. Returning to Joshimath he took up a phototheodolite and went south to survey the Rinti glacier and the saddle between Trisul and Nanda Ghunti.

There are four lakes in the municipality: Lake Oberaar, Lake Grimsel, Lake Räterichsboden and Lake Gelmer. In the western part of the municipality are the mountains Schreckhorn, Lauteraarhorn, Finsteraarhorn, Agassizhorn and Sidelhorn. Guttannen also includes Finsteraar Glacier, Lauteraar Glacier, Unteraar Glacier, Grueben Glacier, and Bächli Glacier. By Swiss standards, the municipality is large in area; by comparison it is larger than the entire Canton of Appenzell Innerrhoden.

It is about long, and is largely within the Tongass National Forest. Ocean liner and Taku Glacier in art for Canadian Pacific The glacier was originally named Schultze Glacier in 1883 and the Foster Glacier in 1890, but Taku, the name the local Tlingit natives had for the glacier, eventually stuck. It is nestled in the Coast Mountains and originates in the Juneau Icefield.

Eldorado Glacier is on the south slopes of Eldorado Peak, North Cascades National Park, in the U.S. state of Washington. The glacier is approximately in length, in width at its terminus and descends from . Eldorado Glacier is connected to Inspiration Glacier on its upper slopes. Glacial melt waters from Eldorado Glacier flow south over Roush Creek Falls, which at , is one of the tallest waterfalls in Washington.

Lipen Glacier (, ) is a 5 km long and 3.5 km wide glacier draining the east slopes of the Trojan Range on Anvers Island in the Palmer Archipelago, Antarctica. Situated east of Iliad Glacier and north of Rhesus Glacier. Flowing northeastwards into the head of Patagonia Bay east of Gourdon Peninsula and west of Thompson Peninsula. The glacier is named after the settlement of Lipen in northwestern Bulgaria.

Bozhinov Glacier (, ) is the 5 km long and 2.5 km wide glacier on Danco Coast in Graham Land on the Antarctic Peninsula situated north of Krebs Glacier and south of Nobile Glacier. Flowing westwards to enter Gerlache Strait at Kapisturia Cove in Charlotte Bay. The glacier is named for the Bulgarian pioneer of aviation Georgi Bozhinov (1879-1955) whose innovative aircraft was patented in France in 1912.

Both the glacier drain down to Bhagirathi River near Gangotri. On the southern side Jogin Glacier joins Khatling Glacier so is Ratangiran Glacier. From Khatling Glacier emerges Bhilangana River that also joins Bhgirathi river near Tehri one of the main tributaries of river Ganga. Bhagirathi joins the Alaknanda River the other main tributaries of river Ganga at Dev Prayag and called Ganga there after.

Bersame Glacier (, ) is the 2.4 km long and 1.5 km wide glacier on the west side of Urda Ridge on Clarence Island in the South Shetland Islands, Antarctica situated northeast of Giridava Glacier. It drains the slopes of Mount Llana, flows northwestwards and enters the Southern Ocean northeast of the terminus of Giridava Glacier. The glacier is named after the Thracian settlement of Bersame in Southeastern Bulgaria.

Both the glacier drain down to Bhagirathi River near Gangotri. On the southern side Jogin Glacier joins Khatling Glacier so is Ratangiran Glacier. From Khatling Glacier emerges Bhilangana River that also joins Bhgirathi river near Tehri one of the main tributaries of river Ganga. Bhagirathi joins the Alaknanda River the other main tributaries of river Ganga at Dev Prayag and called Ganga there after.

Norman Clyde Glacier is a small glacier located in the crest of the Sierra Nevada Range in the John Muir Wilderness of Inyo National Forest in Inyo County, California. The glacier is northwest of Norman Clyde Peak () and both are named after California mountaineer Norman Clyde. A small ridge separates the glacier from the adjacent but larger Middle Palisade Glacier located less than to the southeast.

Topographic map of Smith Island. Dragoman Glacier (, ) is a long glacier on Smith Island, South Shetland Islands draining the southeast slopes of Imeon Range southeast of Zavet Saddle and south of the summit Mount Foster. It is situated southeast of Bistra Glacier, southwest of Landreth Glacier and northeast of Armira Glacier, and flows southeastward into Ivan Asen Cove, Osmar Strait. Bulgarian early mapping in 2009.

Mondor Glacier () is a glacier long flowing southwest from the head of Depot Glacier into Duse Bay, Trinity Peninsula, Antarctica. This glacier and Depot Glacier together fill the depression between Hope Bay and Duse Bay which marks the northern limit of Tabarin Peninsula. The glacier was mapped in 1946 and 1956 by the Falkland Islands Dependencies Survey (FIDS), who named the feature in association with Tabarin Peninsula. "Operation Tabarin" (the forerunner of FIDS) was derived from the "Bal Tabarin" in Paris.

Gaussiran Glacier is a glacier in the eastern part of the Britannia Range, Antarctica. It drains north from the saddle with Merrick Glacier to a juncture with Darwin Glacier between the Cranfield Icefalls and the Nebraska Peaks. It is separated from Alley Glacier by a series of large rock buttresses, including Robertson Buttress. It was named by the Advisory Committee on Antarctic Names after Lieutenant C.D. Gaussiran, U.S. Navy, a pilot with the VXE-6 detachment at Darwin Glacier Field Camp, 1978–79.

The Muir Glacier in 1994 The Muir Glacier was named after John Muir, the naturalist, who identified it in 1889. The Muir Glacier was once a tide water glacier with a width of , a length of , and a height of . It has now turned into terrestrial glacier; it has receded and does not flow into the sea. Its retreat has been very rapid and well- documented since its Little Ice Age maximum position at the mouth of Glacier Bay around 1780.

Svetovrachene Glacier (, ) is the 7.5 km long and 4 km wide glacier on Brabant Island in the Palmer Archipelago, Antarctica situated northeast of lower Malpighi Glacier, southeast of Laënnec Glacier and south of Mitev Glacier. It drains the east and south slopes of Taran Plateau and the south slopes of Avroleva Heights, flows southeastwards between Basarbovo Ridge and Einthoven Hill, and enters Pampa Passage northeast of Bov Point. The glacier is named after the settlement of Svetovrachene in Western Bulgaria.

The Morteratsch Glacier (Romansh: Vadret da Morteratsch) is the largest glacier by area in the Bernina Range of the Bündner Alps in Switzerland. It is, just after the Pasterze Glacier and Gepatschferner, the third largest and by volume (1.2 km3) the most massive glacier in the eastern alps. The Morteratsch Glacier is a typical valley glacier with a pronounced ice front. The accumulation zone lies between the peaks of Piz Morteratsch, Piz Bernina, Crast' Agüzza, Piz Argient, Piz Zupò and Bellavista.

Herbst Glacier is located in the US state of Montana in Glacier National Park. The glacier is northeast of Mount Custer and lies above Lake Nooney at an elevation between and above sea level. Immediately east of the Continental Divide, the glacier covers an area of approximately and does not meet the threshold of often cited as being the minimum size to qualify as an active glacier. Between 1966 and 2005, the glacier lost almost 70 percent of its acreage.

Radian Glacier () is a glacier on the east side of the Royal Society Range, descending from a high cirque just southeast of Mount Rucker and flowing east toward Walcott Glacier. In the measurements made of this glacier by the Victoria University of Wellington Antarctic Expedition (VUWAE) (1960–61), one of the survey angles, by chance, was exactly one radian, and the glacier came to be referred to by this term. Radian Ridge () is a ridge named in association with Radian Glacier.

Ahern Glacier is in Glacier National Park in the U.S. state of Montana. The glacier was named after George Patrick Ahern. Ahern Glacier is situated on a ridge between Ipasha Peak to the north and Ahern Peak to the south at an elevation between and above sea level, immediately east of the Continental Divide. Meltwater from the glacier feeds Ahern Glacier Falls, a waterfall which descends an estimated in one sheer drop to a talus slope below en route to Helen Lake.

Map of Sentinel Range. Fonfon Glacier (, ) is the 4 km long and 2.3 km wide glacier on the east side of the main crest of north-central Sentinel Range in Ellsworth Mountains, Antarctica. It is situated north of Gerila Glacier and south of the head of Embree Glacier. The glacier drains the northeast slopes of the northern summit of Long Gables Peak and the southeast slopes of Mount Anderson, flows northeastwards and joins upper Ellen Glacier southeast of Eyer Peak.

The Gauli Glacier () is a long glacier (2005) in the Bernese Alps in the canton of Bern in Switzerland. In 1973, it had an area of . The glacier is famous for the 1946 C-53 Skytrooper crash on the Gauli Glacier and the following rescue mission, which was the first carried out by an aircraft (Fieseler Storch) landing on a glacier. A lake is located at the bottom of the glacier, at a height of 2,146 metres above sea level.

Hoonah Tlingit Tribal House artist Kaachyaas, "Tears of the Glacier" A Tlingit trail marker in the Glacier Bay Park and Preserve The Tlingits regard Glacier Bay as their sacred homeland. The National Park Service takes the view that "Glacier Bay National Park is the spiritual homeland of the Huna Tlingit, and Glacier Bay National Preserve is the homeland of the Ghunaaxhoo Kwaan unit of the Yakutat Tlingit Tribe". The tribes' oral history supports that they were pushed out and migrated south when the glacier advanced. They moved back to the area when the Glacier retreated in the 1880s.

Tyndall Glacier is a small cirque glacier in Rocky Mountain National Park in the U.S. state of Colorado. Tyndall Glacier is on the east side of the Continental Divide and in a cirque to the north of Hallett Peak. Tyndall Glacier is both an ice and a rock glacier, with the lower portions of the glacier being composed primarily of rock debris and a small portion of ice. Tyndall Glacier is named after John Tyndall, an Irish scientist and Alpine mountaineer who in 1861 first ascended the Weisshorn and made an early attempt on the Matterhorn prior to its first ascent.

Irwin Glacier () is a steep tributary glacier in the Bowers Mountains of Antarctica, draining northeast from Edlin Névé and at the terminus coalescing with Montigny Glacier (from the north), with which it enters the larger Graveson Glacier. The glacier was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for Carlisle S. Irwin, a former glaciologist who participated in the study of Meserve Glacier in 1966–67. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

Of these more recent glaciers, the largest is Teton Glacier, which sits below the northeast face of Grand Teton. Teton Glacier is long and wide, and nearly surrounded by the tallest summits in the range. Teton Glacier is also the best studied glacier in the range, and researchers concluded in 2005 that the glacier could disappear in 30 to 75 years. West of the Cathedral Group near Hurricane Pass, Schoolroom Glacier is tiny but has well defined terminal and lateral moraines, a small proglacial lake and other typical glacier features in close proximity to each other.

The Braldu River is a long river, that originates from the Baltoro Glacier and flows to the west where it receives melt waters from the Biafo Glacier. The Baltoro Glacier and the Biafo Glacier are among the largest glaciers outside the polar regions. The Baltoro Glacier give rise to the four Eight-thousanders mountain peaks, among them is the K2 , the second highest mountain peak of the world. The Biafo Glacier holds the Snow Lake, which is 61 mile (100 km) river of ice, it is among the world's longest continuous glacier systems outside of the polar regions.

To the south of the Karpinsky Glacier lies the University Glacier, which reaches a height of 806 m.

Akuliarutsip Sermerssua, also known as Nordenskiöld Glacier, (), is a large glacier located on the east coast of Greenland.

Eugenie Glacier is a glacier on central Ellesmere Island, Nunavut, Canada. It rises to approximately above sea level.

Panmah Glacier is a glacier in Gilgit-Baltistan, Pakistan. It is included in the Central Karakoram National Park.

Between 1966 and 2005, Gem Glacier lost 30 percent of its acreage and Grinnell Glacier lost 40 percent.

White Glacier is located on the north slopes of Mount Tom in the Olympic Mountains and Olympic National Park in the U.S. state of Washington. The main portion of the glacier heads at around in a cirque just under the summit rocks, while the westernmost section of White Glacier is partially separated from the rest of the glacier by several small ridges of rock and flows straight north. The principle portion of the glacier flows north as well, with a glacier toe descending to around where the toe turns northeast to its terminus at . Steep ridges of rock separate an eastern portion of the White Glacier from the Blue Glacier cirque on adjacent Mount Olympus, to the east.

Erskine Glacier () is a glacier long on the west coast of Graham Land, flowing west into Darbel Bay to the north of Hopkins Glacier. It was first surveyed by the Falkland Islands Dependencies Survey (FIDS) in 1946–47, and named "West Gould Glacier". With East Gould Glacier it was reported to fill a transverse depression across Graham Land, but further survey in 1957 showed no close topographical alignment between the two. The name Gould has been limited to the east glacier and an entirely new name, for Angus B. Erskine, leader of the first FIDS party to travel down the glacier and to survey it in detail, has been approved for the west glacier.

The Theodul Glacier (also spelled Theodule Glacier; , ) is a glacier of the Alps, located south of Zermatt in the canton of Valais. It lies on the Swiss side of the Pennine Alps, although its upper basin touches the Italian region of the Aosta Valley. The glacier descends from the west side of the Breithorn () and splits into two diverging branches above Gandegg: the Upper Theodul Glacier (Oberer Theodulgletscher), spilling on a high plateau near Trockener Steg, together with the Furgg Glacier, and the Lower Theodul Glacier (Unterer Theodulgletscher), reaching a height of about above the Gorner Glacier. Both branches are part of the Rhone basin, through the rivers Gornera, Mattervispa, and Vispa.

There are four glaciers around Yogeshwar two on the northern side and two on the southern side. On the southern side Swetvarn Glacier on the south west side and Shyamvarn Glacier on the south east side both these glacier joins Raktvarn Glacier which itself ultimately drains near Gangotri glacier from where emerges Bhagirathi river the main tributaries of river Ganga. On the Northern side, Gulligad Glacier on the north west side and Lambigad Glacier on the north east side both this glacier drains down to Jadh Ganga which also met Bhagirathi river near Bharionghati. Bhagirathi joins the Alaknanda River the other main tributaries of river Ganga at Dev Prayag and called Ganga there after.

The Glacier Park Company, a subsidiary of the Great Northern Railway (GN), constructed and operated hotels, chalets, and other visitor facilities in Glacier National Park, Montana and Waterton Lakes National Park, Alberta from the 1910s through 1960. Operating as a concessionaire of the National Park Service, the company operated from a summer base in East Glacier Park, Montana, near the company's flagship Glacier Park Hotel; winter headquarters were in St. Paul, Minnesota. Originally known as the Glacier Park Hotel Company, the corporate name was shortened to Glacier Park Company in 1943. During the early years of the Glacier Park Company's operation, its facilities were primarily geared to serve tourists who arrived in Glacier on the Great Northern's passenger trains, which stopped at a station adjacent to Glacier Park Hotel.

Bernardo Glacier is one of the largest glaciers in the Southern Patagonian Ice Field. It is located northeast of Témpano Glacier, within Bernardo O'Higgins National Park in Chile. The glacier flows westward Bernardo Fjord.

Clark Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation around . Clark Glacier is just to the southwest of South Sister, a dormant stratovolcano.

Bend Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation around . Bend Glacier is just to the north of Broken Top, an extinct stratovolcano.

Mountaineer Glacier is in the U.S. state of Montana. The glacier is situated in the Mission Mountains at an elevation of above sea level and is north of Mountaineer Peak. The glacier covers approximately .

Sunrise Glacier is in the U.S. state of Montana. Sunrise Glacier is situated in the Mission Mountains at an elevation of above sea level and is east of Mount Shoemaker. The glacier covers approximately .

Kirkby Glacier is a glacier, in length. This glacier drains the central Anare Mountains of Antarctica and flows northwest to the sea from Cape North, and just north of Arthurson Bluff, northern Victoria Land.

Tavlebreen (The Slate Glacier) is a glacier in Nordenskiöld Land at Spitsbergen, Svalbard. The glacier is located between Sinaiberget and Lagerlöfhøgda, flowing from Lovberget towards Passdalen. It has a length of about five kilometers.

Gull Glacier in alt=Latitude. 81.4121°, Longitude. -77.4132° Gull Glacier is a glacier in the Osborn Range of north-central Ellesmere Island, Nunavut, Canada. It lies in the Tanquary Fiord in Quttinirpaaq National Park.

Buxton Glacier () is a glacier flowing northeast into St Andrews Bay, South Georgia. This glacier was named by the United Kingdom Antarctic Place-Names Committee (UK-APC) in 1987 after Buxton and her parents.

Presidentbreen ("The President Glacier") is a glacier in Haakon VII Land at Spitsbergen, Svalbard. The glacier is tributary to the Tinayrebreen, and is surrounded by the mountains of Presidenten, Monarken, Kiliantoppen, Snødomen and Fallièresfjella.

The Chelen Glacier The Chelen Glacier () is a 2.5 km long glacier (2005) situated in the Urner Alps in the canton of Uri in Switzerland. In 1973 it had an area of 3.15 km².

Rossbode Glacier (2020) The Rossbode Glacier () is a 3.5 km long glacier (2005) situated in the Pennine Alps in the canton of Valais in Switzerland. In 1973 it had an area of 1.87 km².

Argosy Glacier () is a glacier about long, flowing east through the Miller Range to enter Marsh Glacier north of Kreiling Mesa. It was named by the New Zealand Geological Survey Antarctic Expedition (1961–62).

Alemania Glacier, also known as Roncagli Glacier, is a glacier located in Alberto de Agostini National Park, Chile. The advance of one of its lobes blocked the drainage of some streams, forming Martinic Lake.

Rijpbreen is a glacier in Gustav V Land at the northern side of Nordaustlandet, Svalbard. The glacier debouches into Bengtssenbukta, a western branch of Rijpfjorden. The glacier is named after Dutch explorer Jan Rijp.

Descent Pass () is a pass leading from Blue Glacier to Ferrar Glacier, in Victoria Land, Antarctica. It was so named by the party led by Albert Armitage of the British National Antarctic Expedition, 1901–04, because of the adventurous descent to Ferrar Glacier made here via Descent Glacier in 1902.

Mefjell Glacier () is a glacier, long, flowing northwest into Gjel Glacier between Menipa Peak and Mefjell Mountain in the Sør Rondane Mountains of Antarctica. It was mapped by Norwegian cartographers in 1957 from air photos taken by U.S. Navy Operation Highjump, 1946–47, and named Mefjellbreen (the middle-mountain glacier).

Green Glacier is a glacier on the west side of Haskell Ridge, flowing north from the Darwin Mountains of Antarctica into Darwin Glacier. It was mapped by the Darwin Glacier Party of the Commonwealth Trans-Antarctic Expedition, 1956–58, who named it because of the green color of its surface.

Sky Top Glacier is in the Beartooth Mountains in the U.S. state of Montana. The glacier is situated at an elevation of in a cirque to the west of Granite Peak, the tallest summit in Montana. The glacier covers approximately and a small proglacial lake is near the glacier terminus.

Foss Glacier is within the Alpine Lakes Wilderness of Snoqualmie National Forest in the U.S. state of Washington and is on the northeast slope of Mount Hinman. Foss Glacier retreated almost between 1950 and 2005. Foss Glacier is separated from the nearly vanished Hinman Glacier to the west by a ridge.

The glacier is being monitored using remote sensing equipment and repeat photography, where images of the glacier are taken from identical locations periodically. Tree ring samples have also been used previously to determine the extent of glacier retreat. Between 1966 and 2005, Agassiz Glacier lost a third of its surface area.

Vulture Peak () is located in the Livingston Range, Glacier National Park in the U.S. state of Montana. The Vulture Glacier is located on the southern flanks of the mountain, while the Two Ocean Glacier is immediately to the north. Vulture Peak is the thirteenth highest summit in Glacier National Park.

On the southern side lies Bethartoli Glacier. On the western side lies Ronti Glacier and Nanda Ghunti Glacier. All this Glacier drains down to Dhauli Ganga one of the main tributaries of river Alaknanda River. Dhauli Ganga later joins Alaknanda River at Vishnu Prayag the other main tributaries of river Ganga.

Blackwelder Glacier () is a pocket glacier, wide and long, between Salmon Hill and Hobbs Glacier in Victoria Land. The glacier was studied during U.S. Navy Operation Deepfreeze, 1957–58, by Troy L. Pewe and was named by him for Eliot Blackwelder, former head of the Geology Department at Stanford University.

The glacier was photographed from the air by U.S. Navy Operation Highjump in January 1947. It was charted by the French Antarctic Expedition, 1949–51, and named after d'Urville's flagship, the Astrolabe. The Astrolabe Glacier Tongue () is a prominent glacier tongue about wide and long, extending northeast from Astrolabe Glacier.

The recently abandoned settlement of Sermermiut (which means 'place of the glacier people') lies just to the north of the glacier, much nearer than Ilulissat. The glacier is sometimes referred to as Ilulissat Glacier. This form simply replaces Jakobshavn with Ilulissat because of the change in the name of the town.

Christian IV Glacier ( or Kong Christian den IV's Gletscher) is a large glacier on the east coast of the Greenland ice sheet. It is named after King Christian IV of Denmark (1577 – 1648). Administratively this glacier is part of the Sermersooq Municipality.Google Earth The area surrounding Christian IV Glacier is uninhabited.

Chocolate Glacier has resumed retreating since and has given back , nearing its previously recorded minimal length. The current terminus at 1800 m is still the lowest of the east side glacier. Chocolate Glacier remains heavily crevassed and active to 1900 m. The lowest 300 m of the glacier are stagnant.

Several secured paths allow pedestrians to walk on the glacier. Snow buses are also operated on the glacier. In July 2017, the frozen bodies of a Swiss couple who went missing in 1942 were discovered on the glacier by a local ski-resort employee, their bodies exposed by the receding glacier.

On the southern side lies Bethartoli Glacier. On the western side lies Ronti Glacier and Nanda Ghunti Glacier. All this Glacier drains down to Dhauli Ganga one of the main tributaries of river Alaknanda River. Dhauli Ganga later joins Alaknanda River at Vishnu Prayag the other main tributaries of river Ganga.

Sandy Glacier is an alpine glacier located on the west slope of Mount Hood in the U.S. state of Oregon. It extends in elevation from about . The glacier is the source of Muddy Fork, a tributary of the Sandy River. The upper extent of the glacier is known for extensive crevasses.

The village was known as Weheka until the 1940s, when the name of the post office was changed to Fox Glacier, after the nearby glacier of the same name. The glacier was given the name of Fox Glacier in 1872 after a visit by then New Zealand premier, William Fox.

Renfrew Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation generally above . Renfrew Glacier is on the northwest slopes of Middle Sister, an extinct stratovolcano.

Jefferson Park Glacier is located in the U.S. state of Oregon. The glacier is situated in the Cascade Range on the northwest slopes of Mount Jefferson. Jefferson Park Glacier is situated at an elevation between .

Terminal moraines mark the maximum advance of the glacier. Recessional moraines are small ridges left as a glacier pauses during its retreat. After a glacier retreats, the end moraine may be destroyed by postglacial erosion.

Skilfonna ("The Divide Glacier") is a glacier in Sørkapp Land at Spitsbergen, Svalbard. It is located west of Russefjella, and separates the glacier of Hedgehogfonna from Vasil'evbreen. The mountains of Brendetoppane separate Skilfonna from Svalisbreen.

Angelbreen (Fish Hook Glacier) is a glacier in Andrée Land at Spitsbergen, Svalbard. It is located between Skuggefjellet and Skirshorg, at the western side of Vestfjorddalen. The shape of the glacier resembles a fish hook.

Green Lake is located in Glacier National Park, in the U. S. state of Montana. The lake is near the southern border of Glacier National Park, midway between Marias Pass and East Glacier Park, Montana.

The Changtse Glacier flows north into the East Rongbuk Glacier. It is possible that the third highest lake in the worldThe Highest Lake in the World: 3. "Changtse Pool" is in the Changtse Glacier at .

Varderyggfonna is a glacier in Wedel Jarlsberg Land at Spitsbergen, Svalbard. The glacier has a length of about 3.5 kilometers, is part of the Recherchebreen glacier complex, and is located between Konglomeratfjellet, Haugknatten and Varderyggen.

An alternate name is Kagheltnu Li'a. Kahiltna Glacier is the longest glacier in the Alaska Range at in length.

Aleksiev Glacier on Nordenskjöld Coast in Graham Land, Antarctica is named after Rayko Aleksiev.Aleksiev Glacier. SCAR Composite Antarctic Gazetteer.

The Davidson Glacier is a large valley glacier near Haines, Alaska that finds its source in the Chilkat Range.

The glacier is named after Swedish polar explorer Alfred Gabriel Nathorst. A former name of the glacier was Leirbreen.

Ice streams that drain the Greenland ice sheet into the sea include Helheim Glacier, Jakobshavn Isbræ and Kangerdlugssuaq Glacier.

The south steep and rocky face rises above the Wenden Glacier. The east side overlooks a glacier named Firnalpeligletscher.

In the east flows the Nangpa glacier. On the northern slope lies the feeding area of the Shalong glacier.

Both the Maclure Glacier and the Lyell Glacier, located nearby on Mount Lyell, have retreated since their first discovery.

Egeberg Glacier is a small glacier between Scott Keltie Glacier and Dugdale Glacier, flowing into the west side of Robertson Bay, Victoria Land, Antarctica. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare. This geographical feature was first charted by the British Antarctic Expedition 1898–1900, under C.E. Borchgrevink, who named it for Consul Westye Egeberg of Christiania (now Oslo), Norway. In the area surrounding Egeberg Glacier there are unusually many named ice formations.

Gentle Glacier () is a small glacier lobe, to the east and immediately below Forecastle Summit, which drains south into deglaciated Barnacle Valley in the Convoy Range of Victoria Land, Antarctica. Though a part of the Northwind Glacier – Fry Glacier system, this diminished glacier flows back into Barnacle Valley. The name was proposed by New Zealand geologist Christopher J. Burgess and describes the glacier, but also the excellent helicopter support provided to his 1976–77 field party by U.S. Navy helicopters, "Gentle" being their code name.

Satellite image of Thurston Island Savage Glacier () is a glacier at the east end of Thurston Island, lying south of Tierney Peninsula and flowing east to Seraph Bay. The glacier was discovered on helicopter flights from the USS Glacier and Burton Island by personnel of the U.S. Navy Bellingshausen Sea Expedition in February 1960. The Advisory Committee on Antarctic Names named the glacier for Lieutenant John Savage, U.S. Navy, dental officer aboard the Glacier, who assisted in establishing geodetic control points in the area.

Mountain, plus Bow Lake Crowfoot Glacier is located in Banff National Park, Alberta, Canada, northwest of Lake Louise, and can be viewed from the Icefields Parkway. The glacier is situated on the northeastern flank of Crowfoot Mountain. Crowfoot Glacier is east of the continental divide, and runoff from the glacier supplies water to the Bow River. The glacier has retreated since the end of the Little Ice Age and now has lost one entire lobe; it therefore no longer resembles the glacier which early explorers named.

From 1980–2012 the mean cumulative mass loss of glaciers reporting mass balance to the World Glacier Monitoring Service is −16 m. This includes 23 consecutive years of negative mass balances. Chart of annual and cumulative glacier mass balance from World Glacier Monitoring Service Data A glacier with a sustained negative balance is out of equilibrium and will retreat, while one with a sustained positive balance is out of equilibrium and will advance. Glacier retreat results in the loss of the low elevation region of the glacier.

Pirogov Glacier (, ) is a 5 km long and 1.5 km wide glacier situated south of Djerassi Glacier, west of the head of Mackenzie Glacier and northwest of Balanstra Glacier on Brabant Island in the Palmer Archipelago, Antarctica. It drains the south-southwest slopes of Mount Parry and flows westwards to enter Dallmann Bay south of Minot Point. The glacier is named for the Russian scientist and surgeon Nikolay Pirogov (1810-1881) who developed modern health care in Bulgaria during the 1877-78 Russo-Turkish War.

Athabasca Glacier in July 2020 The Athabasca Glacier is one of the six principal 'toes' of the Columbia Icefield, located in the Canadian Rockies. The glacier currently loses depth at a rate of about per year and has receded more than and lost over half of its volume in the past 125 years. Easily accessible, it is the most visited glacier in North America. The leading edge of the glacier is within easy walking distance; however, travel onto the glacier is not recommended unless properly equipped.

Inspiration Glacier is on the east slopes of Eldorado Peak, North Cascades National Park in the U.S. state of Washington. The glacier is approximately in length, in width at its terminus and descends from . Inspiration Glacier lies in a cirque with Eldorado Peak to the west, the arête known as Tepeh Towers to the northwest and Klawatti Peak to the northeast. Inspiration Glacier is connected to the Eldorado Glacier to the south and partially separated by the Tepeh Towers from the McAllister Glacier to the north.

The source of the Hoh River is meltwater from the Hoh Glacier on the northeast side of Mount Olympus. The river flows north then west, curving around the north side of the mountain. It collects headwater tributaries from other glaciers on Mount Olympus such as the Ice River, which flows from the Ice River Glacier, and Glacier Creek, which flows from Blue Glacier and White Glacier. Mount Tom Creek, a tributary which joins the Hoh farther downstream, flows from the White Glacier as well.

The lower end of the glacier The Fiescher Glacier (Fieschergletscher in German) is a valley glacier on the south side of the Bernese Alps in the canton of Valais, Switzerland. in length, it is the second longest glacier in the Alps. The glacier covers an area of . The starting point of the Fiescher Glacier is above sea level, on the eastern slope of the Fiescherhorn, it is flanked to the west by the Grünhorn and Gross Wannenhorn and to the east by the Finsteraarhorn.

Seamen from the USS Rombach exploring the glacier in March 1953. Although there are many negative effects of the recession of the Mendenhall Glacier and glaciers in general, there are also a few positive outcomes. With the retreat of the Mendenhall Glacier, the Mendenhall Lake has formed. The lake is a result of the run-off from the glacier and is increasing in size as the glacier continues to retreat.

Merrick Glacier () is a steep tributary glacier just east of Sennet Glacier in the Britannia Range in Antarctica, descending southwestward to enter Byrd Glacier at the west end of Horney Bluff. It was named by the Advisory Committee on Antarctic Names, in association with nearby Byrd Glacier, for , a cargo ship (Central Group of Task Force 68) of U.S. Navy Operation Highjump, 1946–47, led by Admiral Byrd.

Deming Glacier is located on Mount Baker in the North Cascades of the U.S. state of Washington. Between 1850 and 1950, Deming Glacier retreated . During a cooler and wetter period from 1950 to 1979, the glacier advanced but between 1980 and 2006 retreated back . Situated on the southwest slopes of Mount Baker, Deming Glacier is bordered by the Easton Glacier to the east and the Black Buttes ridge to the west.

Location of Oscar II Coast on Antarctic Peninsula. Lesicheri Glacier (, ) is the 7 km long and 3 km wide glacier on Oscar II Coast in Graham Land situated west of Minzuhar Glacier and northeast of Erden Glacier. It drains the southeast slopes of Forbidden Plateau, and flows southeastwards to join Jorum Glacier west of Yordanov Nunatak. The feature is named after the settlement of Lesicheri in Northern Bulgaria.

Location of Nordenskjöld Coast on Antarctic Peninsula. Enravota Glacier (, ) is the 10 km long and 3.5 km wide glacier on Nordenskjöld Coast in Graham Land situated southwest of Vrachesh Glacier and north of lower Drygalski Glacier. It drains the south slopes of Ruth Ridge, and flows southeastwards to join Drygalski Glacier east of Bekker Nunataks. The feature is named after the Bulgarian prince St. Boyan-Enravota (9th century).

The Meares Glacier is a large and only tidewater glacier at the head of Unakwik Inlet in Chugach National Forest, Alaska. The glacier is one of the many in Prince William Sound, and is about 79.6 miles (128 km) east of Anchorage. The glacier is named for eighteenth century British naval captain John Meares. The face of the glacier is one mile (1.6 km) wide where it calves into the inlet.

The Knud Rasmussen Glacier is located in the far northwest of Greenland, to the north of the Thule Air Base. It is one of four large glaciers which feeds the Wolstenholme Fjord (sometimes referred to as "the world's largest ice machine"). The other glaciers are the Salisbury Glacier, the Chamberlin Glacier, and the Harald Moltke Glacier. The Knud Rasmussen Glacier is over in length and is approximately in width.

The Harald Moltke Glacier is located in the far northwest of Greenland, to the north of the Thule Air Base. It is one of four large glaciers which feeds the Wolstenholme Fjord (sometimes referred to as "the world's largest ice machine"). The other glaciers are the Salisbury Glacier, the Chamberlin Glacier, and the Knud Rasmussen Glacier. The Harald Moltke Glacier is over in length and is approximately in width.

Balanstra Glacier (, ) is the 12 km long and 4 km wide glacier on Brabant Island in the Palmer Archipelago, Antarctica situated northeast of Hippocrates Glacier and southwest of Mackenzie Glacier. It drains the southeast slopes of Stribog Mountains, flows east-southeastwards and enters Pampa Passage south of Momino Point and north of Pinel Point. The glacier is named after the ancient Roman station of Balanstra in Western Bulgaria.

Coleman Glacier is located on Mount Baker in the North Cascades of the U.S. state of Washington. Between 1850 and 1950, Coleman Glacier retreated . During a cooler and wetter period from 1950 to 1979, the glacier advanced but between 1980 and 2006 retreated back . Situated on the west slopes of Mount Baker, Coleman Glacier is bordered by the Roosevelt Glacier to the north and the Heliotrope Ridge to the south.

Zbelsurd Glacier (, ) is the 2.25 km long and 1.6 km wide glacier on the west side of Brugmann Mountains on Liège Island in the Palmer Archipelago, Antarctica. It is situated southwest of Sigmen Glacier and north-northeast of Pleystor Glacier, draining the northwest slopes of Pavlov Peak and the north slopes of Mishev Peak, and flowing northwestwards into Bolbabria Cove. The glacier is named after the Thracian god Zbelsurd.

Honnør Glacier () is a glacier flowing to the east side of Lützow-Holm Bay, Antarctica, to the north of the Byvågåsane Peaks. A glacier tongue extending seaward from this feature was mapped by the Lars Christensen Expedition 1936–37 and named Honnørbrygga (the honor wharf). The Japanese Antarctic Research Expedition, 1957–62, found the glacier tongue had broken off but amended the original naming to apply to the glacier.

Rubble Glacier is an ice-filled valley in the Palmer Land region of the Antarctic Peninsula. It is surrounded by Giza Peak and the ridge connecting it to Baily Ridge to the north and Elephant Ridge to the south. Rubble Glacier is referred to as "Man-Pack Glacier" in scientific reports of the early 1960s, but is now descriptively referred to as Rubble Glacier or sometimes as "Louis Glacier".

Location of Oscar II Coast on Antarctic Peninsula. Paspal Glacier (, ) is the 14.5 km long and 6.5 km wide glacier on Oscar II Coast, Graham Land in Antarctica situated southeast of Montgolfier Glacier and west of Hektoria Glacier. Draining from the southeast slopes of Forbidden Plateau and flowing southeastwards between Zagreus Ridge and Dugerjav Peak to join Green Glacier. The feature is named after the settlement of Paspal in southern Bulgaria.

Cloud Peak Glacier is in the Bighorn Mountains in the northcentral section of the U.S. state of Wyoming. Centered within the Cloud Peak Wilderness of Bighorn National Forest, Cloud Peak Glacier is the only active glacier in the Bighorn Mountains. The glacier is in a deep cirque immediately northeast of Cloud Peak, the highest peak in the Bighorn Mountains. Cloud Peak Glacier lies at approximately above sea level.

Mount Jackson () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Mount Jackson is the fourth tallest mountain in Glacier National Park and it is situated on the Continental Divide. Both the mountain and its namesake Jackson Glacier are easily seen from the Going-to-the-Sun Road. Harrison Glacier, the park's largest remaining glacier, is located on the mountain's southern flank.

Slightly above the glacier splitting is the Theodul Pass, crossing the border between Switzerland and Italy, and connecting Zermatt to Breuil- Cervinia. On the west, the Theodul Glacier is overlooked by the Matterhorn. Until about 1980s the Lower Theodul Glacier was still connected to the Gorner Glacier and one of its tributaries. The upper section of the Theodul Glacier consists of a flat plateau at around 3,800 metres, named Breithorn Plateau.

Icefall of Khumbu glacier The Khumbu Glacier is located in the Khumbu region of northeastern Nepal between Mount Everest and the Lhotse-Nuptse ridge. With elevations of at its terminus to at its source, it is the world's highest glacier. The Khumbu Glacier is followed for the final part of the trail to one of the Everest Base Camps. The start of the glacier is in the Western Cwm near Everest.

Matanuska Glacier flows about per day. Due to ablation of the lower glacier, , the location of the glacier terminus changed little over the previous three decades. There is an Alaska State Parks facility, the Matanuska Glacier State Recreation Site, a park with trails and a small campground.Matanuska Glacie SRS, Alaska Department of Natural Resources The glacier is the eponym of the Alaska Marine Highway ferry M/V Matanuska.

Kolahoi Glacier is a valley glacier in the northwestern Himalayan Range situated 26 kilometers north from Pahalgam and 16 kilometers south from Sonamarg, in the union territory of Jammu and Kashmir. Kolahoi glacier lies at an average elevation of . The highest peak named after the glacier is Kolahoi Peak has an elevation of 5425 meters. The origin of the glacier is below the cirques on the north flank of Kolahoi Peak.

In the case of Helheim Glacier, researchers used satellite images to determine the movement and retreat of the glacier. Satellite images and aerial photographs from the 1950s and 1970s show that the front of the glacier had remained in the same place for decades. In 2001 the glacier began retreating rapidly, and by 2005 the glacier had retreated a total of , accelerating from per day to per day during that period.

On the south western side lies Uttari Chamrao Glacier, Dakshini Chamrao Glacier, Balbala Glacier, Khagyan Glacier and Paschimi Kamet glacier all these glaciers drain their water in the Saraswati River which then joins Alaknanda River at Keshav Prayag near Mana village one of the main tributaries of river Ganga. River Alaknanda merges with river Bhagirathi the other main tributaries of river Ganga at Dev Prayag and called Ganga there after.

The North Mowich Glacier is a glacier located on the northwest flank of Mount Rainier in Washington. It covers and contains 9.5 billion ft3 (269 million m3) of ice. Starting from the foot of Rainier's steep Mowich Face at about , the glacier first consists of two lobes of ice that flow downhill to the northwest. The southern arm of the glacier is connected to the adjacent Edmunds Glacier.

Backstairs Passage Glacier () is a glacier about long, draining east along the north side of Mount Crummer to the Ross Sea. The Magnetic Pole Party, led by Edgeworth David, of the British Antarctic Expedition, 1907–09, ascended this glacier from the Ross Sea, then continued the ascent via Larsen Glacier to the plateau of Victoria Land. So named by David's party because of the circuitous route to get to Larsen Glacier.

Glacier foreland beneath the Langgletscher in Switzerland The region between the current leading edge of the glacier and the moraines of latest maximum is called glacier foreland or glacier forefield. In the Alps this maximum was in 1850 and since then the region has become ice free due to deglaciation. Because of this relative recent development of vegetation and morphodynamic the glacier foreland differs considerably from the surrounding landscape.

Topographic map of Smith Island Dalgopol Glacier (, ) is a long glacier draining the northwest slopes of Imeon Range on Smith Island in the South Shetland Islands, Antarctica. It is situated northeast of Vetrino Glacier and southwest of Kongur Glacier, and flows north of Mount Pisgah and northwest of Mezek Peak into Drake Passage. Bulgarian early mapping in 2009. The glacier is named after the town of Dalgopol in northeastern Bulgaria.

Topographic map of Smith Island. Ovech Glacier (, ; ) is a 3.5 km long glacier on Smith Island, South Shetland Islands draining the southeast slopes of Imeon Range southeast of Drinov Peak and east of Popovo Saddle and Sevlievski Peak. It is situated southeast of Vetrino Glacier and Yablanitsa Glacier, and northeast of Krivodol Glacier, and flows east-southeastward into Nikolov Cove on Boyd Strait. Bulgarian early mapping in 2009.

The Corbassière Glacier (Glacier de Corbassière in French) is a valley glacier in the Grand Combin massif in the Pennine Alps in southwestern Valais. It is long with an average width of slightly more than and covers an area of . The origin of Corbassière Glacier is on the northern slope of the Grand Combin at over above sea level. The glacier tongue currently ends at around above sea level.

Meserve Glacier () is a hanging glacier on the south wall of Wright Valley, in the Asgard Range of Victoria Land, Antarctica, between Bartley Glacier and Hart Glacier. It was named by U.S. geologist Robert Nichols for William Meserve, a geological assistant to Nichols in Wright Valley in the 1959–60 field season.

Heksebreen ("The Witch Glacier") is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of about 3.5 kilometers, and is a tributary glacier to Eidembreen. The glacier is located south in the mountainous district of Trollheimen, and is surrounded by the mountains of Heksefjellet, Runebomma, Trollungen and Stortrollet.

Maine Ridge () is a ridge that extends northwest–southeast between Matataua Glacier and Tedrow Glacier in the Royal Society Range, Antarctica. It was named after the University of Maine, Orono, in association with other features in the immediate area named for educational institutions, such as Emmanuel Glacier, Johns Hopkins Ridge, and Rutgers Glacier.

Tviberi () is a glacier located in the Svaneti Region of Georgia on the southern slopes of the Greater Caucasus Mountain Range. The length of the Tviberi Glacier is and its surface area is . The tongue of the glacier descends to above sea level. Tviberi represents a polisynthetic type of a valley glacier.

Milk Creek Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range on the west slope of Mount Jefferson. Milk Creek Glacier is situated at an elevation between . Milk Creek Glacier is considered stagnant ice and is located immediately west and below the summit of Mount Jefferson.

Koteshwar lies in between two glaciers. On the eastern side lies Swetvarn Glacier and on the western side lies Thelu Glacier. Both these glaciers join Raktavarn Glacier on the south. Finaly Raktvarn drain itself at Gangotri Glacier near Gomukh from there emerges Bhagirathi River one of the main tributaries of river Ganga.

O'Higgins Glacier is a glacier located in Bernardo O'Higgins National Park, Chile. It is one of the principal glaciers of the Southern Patagonian Ice Field. The summit of the active Lautaro volcano is the top of the accumulation zone of the glacier. The bulk of the glacier is part of the icefield plateau.

Kehle Glacier () is a glacier draining the western slopes of the Worcester Range, Antarctica. It is near Mount Speyer and Mount Dawson-Lambton, and flows southwest into Mulock Glacier. The glacier was named by the Advisory Committee on Antarctic Names in 1964 for Ralph Kehle, a glaciologist at Little America V, 1959–60.

Kennicott Glacier on approach to Mount Blackburn. Geologic map depicting the glacier Kennicott Glacier is a glacier in the U.S. state of Alaska. It trends southeast 43 km (27 mi) from Mount Blackburn to its terminus at the head of the Kennicott River in the Wrangell Mountains. It is located in Wrangell-St.

Lee Glacier () is a glacier flowing southeast into Jorda Glacier, in the Churchill Mountains, Antarctica. Mount Frost and Mount Coley are located at its head. The glacier was named in honor of Sandra Lee, a former New Zealand Minister of Conservation, for her contribution to environmental protection in Antarctica and its surrounding waters.

Bering Glacier is a glacier in the U.S. state of Alaska. It currently terminates in Vitus Lake south of Alaska's Wrangell-St. Elias National Park, about from the Gulf of Alaska. Combined with the Bagley Icefield, where the snow that feeds the glacier accumulates, the Bering is the largest glacier in North America.

Hubbard Glacier still has a calving front. The glacier will then expand until the AAR is between 60 and 70 and equilibrium of the non-calving glacier is achieved. The glacier is not very sensitive to climate during the advance as its AAR is quite high, when the terminus shoal is limiting calving.

Headwall of Fourpeaked Glacier with steam and volcanic gases rising through vents on Sept. 20, 2006 Terminus of Fourpeaked Glacier with dark-colored sediment issuing from an elongate tunnel in the ice. Photo taken Sept 20, 2006 Fourpeaked Glacier is a calving glacier covering much of Fourpeaked Mountain, also known as Fourpeaked Volcano.

The Verstancla Glacier () is a 2 km long glacier (2005) situated in the Silvretta Range in the canton of Graubünden in Switzerland. In 1973 it had an area of 1.27 km². The glacier is located north of the Verstanclahorn. It is parallel to the larger Silvretta Glacier lying a few kilometres north.

Middle Palisade Glacier consists of two glaciers in the Sierra Nevada mountains, in the U.S. state of California. Less than southeast of Norman Clyde Glacier and situated at an altitude of , Middle Palisade Glacier is in the John Muir Wilderness of Inyo National Forest. Middle Palisade is immediately west of the glacier.

Topographic map of Smith Island. Kongur Glacier (, ) is a long glacier draining the northwest slopes of Imeon Range on Smith Island in the South Shetland Islands, Antarctica. It is situated northeast of Dalgopol Glacier and southwest of Saparevo Glacier, and flows west of Mount Christi into Drake Passage. Bulgarian early mapping in 2009.

White Salmon Glacier is located on Mount Adams in the U.S. state of Washington. The glacier starts southwest of the summit crater at an elevation of . Ice flows southwest downhill until the glacier's terminus at about elevation. The glacier also contributes ice to the much larger Avalanche Glacier at an elevation of .

China's famous glaciologist Shi Yafeng served as the vice captain. The July 1 Glacier is the first glacier discovered by this team. Due to global warming, the July 1 Glacier is shrinking. On July 24, 2017.

Spørteggbreen is a glacier in the municipality of Luster in Vestland county, Norway. It is the 12th largest glacier in Norway. It lies between the Jostedalsbreen and Harbardsbreen glaciers. The glacier lies inside Breheimen National Park.

Mount Wheeler is surrounded by ice, including the Deville Glacier, Deville Névé, Black Glacier, and Thor Glacier. Precipitation runoff from the mountain and meltwater from its glaciers drains into tributaries of the Incomappleux and Beaver Rivers.

The Brunegg Glacier () is a long glacier (2005) situated in the Pennine Alps in the canton of Valais in Switzerland. In 1973 it had an area of . The glacier is located north of Bishorn and Weisshorn.

Blue Glacier is also thinning as it retreats and between 1987 and 2009 the glacier lost of its depth near its terminus and between in the uppermost sections of the glacier known as the accumulation zone.

A glacier in Antarctica is named after him due to his work in aviation (Henson Glacier: 64'06'S, 60'11'WHenson Glacier)). Henson and Stringfellow were referred to in the 1965 film The Flight of the Phoenix.

Krøkjebreen ("The Bent Glacier") is a glacier in Torell Land at Spitsbergen, Svalbard. It has a length of nine kilometers. Krøkjebreen is part of the Liestølbreen glacier complex, situated between the mountains of Arrheniusfjellet and Wijkberget.

Ramondbreen is a glacier in Wedel Jarlsberg Land at Spitsbergen, Svalbard. The glacier has a length of about two kilometers, and is part of the Recherchebreen glacier complex. It is named after Arctic explorer Gontaud Ramond.

Uludoruk Glacier is a glacier on Mount Uludoruk, one of the Taurus Mountains and the second highest mountain in Turkey. Between 1948 and 2009 the glacier retreated 12m per year, due to climate change in Turkey.

Renardbreen (The Fox Glacier) is a glacier in Wedel Jarlsberg Land at Spitsbergen, Svalbard. The glacier has a length of about . It is located between the ridges of Activekammen and Bohlinryggen, and debouches into Recherche Fjord.

Coming out of the Muir inlet and entering and cruising toward the north along the main Bay, on the west shore are the Gelkie Inlet, Reid Glacier and Lamplugh Glacier fed by Brady Ice field and Brady Glacier, followed by Johns Hopkins Glacier, Margerie Glacier and the Great Pacific Glacier at the head of the Bay. The east shore line has the Queen Inlet with its Carroll Glacier, and the Rendu Inlet with its Rendu Glacier. The Fairweather Range of hills which feeds the Johns Hopkins and Margerie Glaciers form the western boundary of the Glacier Bay and the highest mountains seen here are the Mt. Fairweather (), Mt. Quincy Adams (), Mt. Salisbury (), Mt. Crillon (), Mt. Bertha (), Mt. Abbe () and Mt. Cooper (). The major island, opposite to the Johns Hopkins Inlet, is the Russel Island in the midst of the main channel.

The Glacier National Park Conservancy was established on January 1, 2013 from a merger of the Glacier National Park Fund (established in 1999) and the Glacier Association (established in 1941). The Glacier National Park Fund previously operated as a non-profit fund raising organization whose main goal was to raise money to support various needs of Glacier National Park, headquartered in West Glacier, Montana. In its history, the Glacier National Park Fund raised 3.5 million dollars. The Glacier Association was founded in 1941 and incorporated in 1946 and provided funding from receipts received from book and merchandise sales at not only Glacier National park bookstores and visitor centers, but at other federal facilities including Flathead National Forest, Grant-Kohrs Ranch National Historic Site, Big Hole National Battlefield and the National Bison Range, all of which are located in the state of Montana.

Rivera, A., Acuña, C. and Casassa, G. Glacier variations in central Chile (32°S-41°S). Chapter in Glacier science.

Photo of the Bear Glacier The glacier was part of the closing scene in the film "Insomnia" with Al Pacino.

There is a fairly large glacier, the Navarana Fjord Glacier, at the head of the fjord discharging from the southeast.

Comparing images of the glacier taken in 1914 with those from 2009, indicates that the glacier has experienced extensive retreat.

The glacier persists only on the north flank of Mount Hinman. Repeat photography indicates that Hinman Glacier has retreated significantly.

Thordarhyrna ( ) is one of seven Figure 2.8 shows 7 volcanoes beneath the glacier subglacial volcanoes beneath the Vatnajokull glacier Iceland.

The Biarchedi Glacier () is located on the northeast of Biarchedi Peak in Pakistan. It flows north into the Baltoro Glacier.

Since then Cool Glacier resumed retreating and by 2005 the glacier was within of its minimum length recorded in 1946.

Aphrodite Glacier () is a glacier long flowing north to the east coast of the Antarctic Peninsula west of Victory Nunatak.

Glacier front of the Kongsvegen The Kongsvegen is a glacier, located in west Spitsbergen, Svalbard, north of the Norwegian mainland.

Nordenskiöldbreen (Nordenskiöld Glacier) is a glacier in Spitsbergen, Svalbard. It is named after Finnish geologist Adolf Erik Nordenskiöld (1832–1901).

In 2013, a fourth glacier cave was discovered on the Sandy Glacier, but so far it has not been explored.

Eight of the twelve largest glaciers in New Zealand lie within Aoraki/Mount Cook National Park, all of which terminate at proglacial lakes formed in recent decades due to a sustained period of shrinking. In the area surrounding Aoraki / Mount Cook, the Tasman Glacier, Hooker Glacier, Murchison Glacier, and Mueller Glacier all terminate in lakes, while further north in the park, the Godley Glacier, Classen Glacier, Grey Glacier and Maud Glacier also end in proglacial lakes. Tasman Lake and Hooker Lake are easily accessible via walking tracks and are the only two of these lakes that have official names. At an area of 7 km², Tasman Lake is the largest of the proglacial lakes and hosts boat trips for tourists.

The Drang-Drung Glacier (also called Durung Drung Glacier) is a mountain glacier near the Pensi La mountain pass at the Kargil - Zanaskar Road in the Kargil district of Ladakh in India. The Drang-Drung Glacier is likely to be the largest glacier in Ladakh other than the Siachen Glacier in the Karakoram Range, with a maximum length of at an average elevation of . The glacier lies in the northeastern Himalayan Range known as the Zanskar Range, south of Kargil and east of Srinagar, the capital of Jammu and Kashmir. The Drang-Drung Glacier is a long river of ice and snow, a source of the Stod River which is a tributary of the Zanskar River and the Zanskar River is a tributary of Indus River.

Lost Creek Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation generally above . Lost Creek Glacier is on the northwest slopes of South Sister, a dormant stratovolcano.

Watson Glacier is in Snoqualmie National Forest in the U.S. state of Washington, on the north slope of Mount Watson. Watson Glacier retreated between 1950 and 2007 and is now only in length. Watson Glacier descends from .

Thunder Glacier is located on the northeast slopes of Buckner Mountain, North Cascades National Park in the U.S. state of Washington. The glacier is approximately long and separated from the much larger Boston Glacier by an arete.

Alaska has more than three million lakes. Marshlands and wetland permafrost cover (mostly in northern, western and southwest flatlands). Glacier ice covers about of Alaska. The Bering Glacier is the largest glacier in North America, covering alone.

Hochstetterbreen is a glacier located in Olav V Land on Spitsbergen. Hochstetterbreen is a glacier in Olav V Land on Spitsbergen, Svalbard. It debouches into Hinlopen Strait. The glacier is named after Austrian geographer Ferdinand von Hochstetter.

Garrard Glacier () is a glacier in the Queen Alexandra Range of Antarctica, draining eastward from the névé between Mount Lockwood and Mount Kirkpatrick and entering Beardmore Glacier south of Bell Bluff. It appears that the British Antarctic Expedition, 1910–13, applied the name "Garrard Glacier" to the feature which had been named Bingley Glacier by Ernest Shackleton in 1908. The area was surveyed by the New Zealand Geological Survey Antarctic Expedition (1961–62), who retained Bingley Glacier on the basis of priority and reapplied the name Garrard Glacier to this previously unnamed feature. The name is for Apsley Cherry-Garrard, a zoologist with the British Antarctic Expedition.

Barranco Glacier (once known as the Great Barranco Glacier) is near the summit of Mount Kilimanjaro in Tanzania, on the southwest slope of the peak and is a small remnant of an icecap which once crowned the top of Mount Kilimanjaro. The glacier is situated at an elevation of between . The Great Barranco Glacier was far larger when first documented in the late 19th century and it along with the now extinct Little Barranco Glacier may have been fed by the Furtwängler Glacier which is on the top of the mountain. By 2011, Barranco Glacier was reduced to two small disconnected and dormant ice bodies.

It could be reached from the Baltoro glacier on the Pakistani side of the Karakorams via the Old Muztagh Pass northeast of the Trango Towers. It is however easier to approach the glacier from the Chinese side, starting a long hike at Kashgar on the Karakoram Highway and finally passing K2's northern base camp. The Glacier is named after Francis Younghusband, who was the first person to pass the Old Mustagh Pass and thus enter the Sarpo Laggo region. There is another glacier not far away, also named after him: Younghusband glacier (also known as Biango glacier) flows from Muztagh Tower towards the Baltoro Glacier.

Location of Clarence Island in the South Shetland Islands. Clarence Island seen from northeast with (left to right) Cape Bowles; Dobrodan Glacier and Highton Glacier surmounted by Duclos-Guyot Bluff and Mount Irving; Treskavets Glacier, Orcho Glacier and Banari Glacier surmounted by Ravelin Ridge; and Cape Lloyd. Duclos-Guyot Bluff (, ‘Vrah Duclos-Guyot’ \'vrah dyu-'klo gi-'yo\\) is the ice-covered peak rising to 1800 m at the south extremity of Urda Ridge on Clarence Island in the South Shetland Islands, Antarctica. It has precipitous and partly ice-free south slopes, and surmounts Skaplizo Glacier to the west and Dobrodan Glacier to the northeast.

The Hubbard Glacier If we begin at the stable retracted position at the end of a tidewater glacier cycle the glacier will have a moderate calving rate and a high AAR, above 70. The glacier will build a terminus shoal of sediment further reducing the calving rate. This will improve the glacier mass balance and the glacier can begin to advance due to this change or an increase in ice flux to the terminus due to increasing snowfall or reduced snow melt. As the advance proceeds the terminus shoal will be pushed in front of the glacier and continue to build, keeping the calving rate low.

Bamchu Glacier on the eastern side joins Milam Glacier from there emerges Goriganga River that later joins the Kali River at Jauljibi. Uttari Nanda Devi Glacier on the western side joins Uttari Rishi Glacier and drains into Rish Ganga. Rishi Ganga met with Dhauliganga River near Rini. Later Dhauli ganga met with Alaknanda at Vishnuprayag.

More than thirty glaciers originate in the icefield, which first formed about 23,000 years ago. Icefield coverage has declined, with a 3% reduction in coverage over a 16-year study period. The park's largest glacier is Bear Glacier. The most accessible glacier, and the only portion of the park accessible by road, is Exit Glacier.

Moubray Glacier is a rather steep glacier flowing south to Moubray Bay from Adare Saddle on Adare Peninsula in Antarctica. It is one of the main contributors of ice to Moubray Piedmont Glacier. The glacier was named by the New Zealand Geological Survey Antarctic Expedition of 1957–58 for its proximity to Moubray Bay.

Gerasimou Glacier () is a steep-walled tributary glacier, long, entering the west side of Shackleton Glacier opposite the Gemini Nunataks, in the Queen Maud Mountains of Antarctica. It was named by the Texas Tech Shackleton Glacier Expedition, 1964–65, for Helen Gerasimou, a polar personnel specialist with the Office of Antarctic Programs, National Science Foundation.

Sakram Glacier on the eastern side joins Milam Glacier from there emerges Goriganga River that later joins the Kali River at Jauljibi. Uttari Nanda Devi Glacier on the western side joins Uttari Rishi Glacier and drains into Rish Ganga. Rishi Ganga met with Dhauliganga River near Rini. Later Dhauli ganga met with Alaknanda at Vishnuprayag.

It has steep and partly ice-free north and west slopes, and surmounts Djerassi Glacier to the north-northwest, Mackenzie Glacier to the east, Balanstra Glacier to the south-southeast and Pirogov Glacier to the southwest. Mount Parry was first ascended by the British Joint Services Expedition led by John Furse on 30 October 1984.

Stuart Glacier lies to the north of Mount Stuart, in the U.S. state of Washington. Stuart Glacier is within the Alpine Lakes Wilderness of Wenatchee National Forest. The glacier is approximately in length, in width at its widest and descends from , where it terminates as an icefall. Less than to the southeast lies Sherpa Glacier.

Dolra is a valley glacier located on the southern slopes of the Greater Caucasus Mountain Range in the Svaneti Region of Georgia. The length of the glacier is and its surface area is . The tongue of the Dolra Glacier descends down to above sea level. The glacier is the source of the river Dolraschala.

On the east side lies Swetvarn Glacier which joins Raktvarn Glacier and Raktvarn drain itself near Gomukh beside Gangotri Glacier and part of Bhagirathi river. Bhagirathi River comes out From the snout of Gangotri Glacier. Bhagirathi joins the Alaknanda River the other main tributaries of river Ganga at Dev Prayag and called Ganga there after.

Bjørlykkebreen (Bjørlykke Glacier) is a glacier in Albert I Land, Spitsbergen, Svalbard. It is a tributary of Lillehöökbreen, and is debouching into the Lilliehöökfjorden. The glacier is named after Norwegian geologist Knut Olai Bjørlykke (1860 – 1946) following a proposal in 1912 by Adolf Hoel who had traversed the glacier in 1909 together with Olaf Holtedahl.

Queest-alb Glacier is in Snoqualmie National Forest in the U.S. state of Washington, on the west slopes of Three Fingers. Queest-alb Glacier is also known as Three Fingers Glacier, but neither name is officially recognized by the United States Geological Survey. The glacier descends from and is a popular location for skiing.

Camping is in between the moraines Kalindi base camp (5560 m) : The glacier splits up. The rout goes north to follow the Kalindi glacier. River camp (4770 m) : The route stops following the main glacier and goes steep up toward Kalindi pass. On the other side the route goes down over a white glacier.

Gangotri Glacier lies from the northern side to eastern side of Kharchakund. On the western side lies Ghanohim Bamak and on the south east lies Yeonbuk Bamak. Yeonbuk and Ghanoim both these glacier joins Gangotri glacier. From the snout of Gangotri Glacier comes out Bhagirathi River one of the main tributaries of river Ganga.

Bakaninbreen merges with Paulabreen before the combined glacier debouches into the bay of Rindersbukta. Bakaninbreen is a glacier in Heer Land at Spitsbergen, Svalbard. It has a length of about 9.5 kilometers, and merges with the glacier of Paulabreen. The glacier is named after a member of the Swedish-Russian Arc-of-Meridian Expedition.

Map of northern Sentinel Range. Yamen Glacier (, ) is the 10 km long and 4 km wide glacier in Gromshin Heights on the east side of northern Sentinel Range in Ellsworth Mountains, Antarctica. It is situated northeast of Vicha Glacier. The glacier drains northeastwards along the north slopes of Branishte Peak and joins Rutford Ice Stream.

In 1997, Kanyon donned a mask and was repackaged as Mortis, a Latin word meaning death. Managed by James Vandenberg, Kanyon feuded with Glacier. Kanyon faced Glacier at Uncensored on March 16 in his pay-per- view debut but lost to the undefeated Glacier. Following the match, Wrath debuted, siding with Kanyon and assaulting Glacier.

Warmer temperatures and changes in precipitation over the past century have thinned the Bering Glacier by several thousand meters. Since 1900 the terminus has retreated as much as . The Bering Glacier exhibits "surges", acceleration events of the flow rate of the glacier, every 20 years or so. During these periods the glacier terminus advances.

The Hugihorn (3,647 m) is a peak of the Bernese Alps, overlooking the Unteraar Glacier in the canton of Bern. It lies south of the Klein Lauteraarhorn, on the range separating the Strahlegg Glacier from the Lauteraar Glacier, both tributaries of the Unteraar Glacier. The mountain was named after the Swiss geologist Franz Joseph Hugi.

Goode Glacier is in North Cascades National Park in the U.S. state of Washington, on the east slopes of Goode Mountain. Goode Glacier is a hanging glacier and is broken into several sections descending from . Goode Glacier sits more than below the summit of Goode Mountain, the tallest peak in North Cascades National Park.

The glacier is located to the northeast of the rounder Imja Tsho lake shown south of centre Lhotse Shar is a glacier of the Himalayas in the Solukhumbu District of Nepal. It adjoins Imja Glacier to the northeast and with Ambulapcha Glacier forms three major glaciers. To the east is Cho Polu (6734m/22,093ft).

Perkins Press, 1912. His mother was a descendant of President Zachary Taylor. The peak is a popular hiking destination with views of the Emmons Glacier, Winthrop Glacier, Inter Glacier, Fryingpan Glacier, Little Tahoma Peak, and views in all directions because the trail is above tree line. The trail starts at the Sunrise Historic District.

In the St. Elias Range, Mount Churchill has erupted explosively within the past 2,000 years. The park's glacial features include Malaspina Glacier, the largest piedmont glacier in North America, Hubbard Glacier, the longest tidewater glacier in Alaska, and Nabesna Glacier, the world's longest valley glacier. The Bagley Icefield covers much of the park's interior, which includes 60% of the permanently ice- covered terrain in Alaska. At the center of the park, the boomtown of Kennecott exploited one of the world's richest deposits of copper from 1903 to 1938.

Bhagirathi Massif or Bhagirathi Group (Hindi: भागीरथी ) is a mountain range of Garhwal Himalaya in Gangotri Glacier Uttarakhand India, It has four peaks between 6856 meter and 6193 meter. The Bhagirathi I summits is 6856 meter or 22493 feet. It was first climbed by A Japanese team in 1980. It is surrounded by Glaciers on four side on the eastern side of the Massif is Vasuki Glacier, on the western side its Gangotri Glacier the main glacier in this area, northern side is surrounded by Chaturangi Glacier and southern side guarded by Swachhhand Glacier.

Location of Hemimont Plateau on the Antarctic Peninsula. Klebelsberg Glacier () is a glacier, long and wide, situated at the south side of Finsterwalder Glacier and flowing from Hemimont Plateau northwestward between Armula Peak and Smilyan Bastion on Graham Land, Antarctica, toward the head of Lallemand Fjord. With Finsterwalder Glacier and Haefeli Glacier, its mouth merges with Sharp Glacier where the latter enters the fjord. It was first surveyed from the plateau in 1946–47 by the Falkland Islands Dependencies Survey, and named by them for Raimund von Klebelsberg, an Austrian glaciologist.

Topographic map of Smith Island. Nosei Glacier (, ) is the steep 1.3 km long and 1 km wide glacier draining the southeast slopes of Imeon Range on Smith Island in the South Shetland Islands, Antarctica. It is situated east of upper Dalgopol Glacier, southeast of Kongur Glacier and southwest of Ritya Glacier, flows eastwards from a part of the main crest between Mezek Peak and Mount Christi, and enters the head of Pakusha Cove on Boyd Strait. The glacier is named after the settlement of Noseite in Northern Bulgaria.

Peyto Glacier and part of the Wapta Icefield as seen from near the Peyto Lake lookout - Mt. Habel in the icefield. The Peyto Glacier is situated in the Canadian Rockies in Banff National Park, Alberta, Canada, approximately northwest of the town of Banff, and can be accessed from the Icefields Parkway. Peyto Glacier is an outflow glacier from the Wapta Icefield, which rests along the Continental divide. The glacier snout is subject to high melt rates from season to season and there is marked surface lowering on several parts of the glacier.

Glaciers are uncommon in the Northern Limestone Alps, and those on the Dachstein — the Hallstätter Gletscher ("Hallstatt glacier"), the Großer Gosaugletscher ("great Gosau glacier") and the Schladminger Gletscher ("Schladming glacier") — are the largest, as well as being the northernmost and the easternmost in the whole of the Alps. Several smaller ice-fields also exist, such as the Kleine Gosaugletscher ("lesser Gosau glacier") and the Schneelochgletscher ("snow-hole glacier"). The glaciers are retreating rapidly, and may disappear entirely within 80 years. The Hallstatt glacier withdrew by 20 m in the year 2003 alone.

Hudson Glacier is located in the US state of Montana in Glacier National Park. The glacier is situated in a cirque immediately to the east of the Continental Divide at an elevation between and above sea level. A half-mile south of Lake Nooney and Lake Wurdeman, Hudson Glacier covers an area of approximately and does not meet the threshold of often cited as being the minimum size to qualify as an active glacier. Between 1966 and 2005, the glacier lost more than 66 percent of its acreage.

Central and southern Sentinel Range map. Cairns Glacier () is a glacier on the west slope of Vinson Massif, Sentinel Range in Antarctica, situated between Branscomb Glacier and Tulaczyk Glacier. It flows along the northwest side of Brichebor Peak southwestwards, and leaving the range together with Tulaczyk Glacier joins Nimitz Glacier southeast of Klenova Peak. The feature was named by US-ACAN (2006) after Stephen Douglas Cairns, research zoologist, Department of Invertebrate Zoology, National Museum of Natural History, Smithsonian Institution, 1985–2006; Board of Associated Editors, Antarctic Research Series, American Geophysical Union, 1990–95.

Jenkins Glacier () is a glacier close south of Risting Glacier, flowing east into the head of Drygalski Fjord in the southeastern part of South Georgia. The glacier was named for Erich von Drygalski by the Second German Antarctic Expedition, 1911–12, under Wilhelm Filchner. To avoid duplication with Drygalski Glacier in Graham Land, also named for Erich von Drygalski, a new name was proposed in 1957 by the UK Antarctic Place-Names Committee. Jenkins Glacier is named for James Travis Jenkins, author of A History of the Whale Fisheries and Bibliography of Whaling.

McAllister Glacier is in a large cirque to the north and east of Dorado Needle, North Cascades National Park, in the U.S. state of Washington. The glacier is approximately in length, in width at its terminus and descends from , where it terminates near a proglacial lake. McAllister Glacier is nearly connected to Inspiration Glacier to the south and the two glaciers are separated by the arête known as Tepeh Towers. Klawatti Peak and an arete extending north from that peak separate McAllister Glacier from the Klawatti Glacier to the east.

The Abruzzi Glacier () is a glacier north of the Baltoro Kangri peak in Gilgit-Baltistan, Pakistan. The glacier joins the Baltoro Glacier (one of the largest glaciers outside the polar region) that flows northwest in the beginning and then turns westward. The glacier provides superb views of K2, the highest peak in Pakistan. The glacier was named in honor of Prince Luigi Amedeo, Duke of the Abruzzi an Italian mountaineer and arctic explorer who led an expedition to the Karakoram mountain range in 1909, including several partial ascents of K2.

Map of northern Sentinel Range. Vicha Glacier (, ) is the 27 km long and 6 km wide glacier in Gromshin Heights on the east side of northern Sentinel Range in Ellsworth Mountains, Antarctica. It is situated northeast of Newcomer Glacier and southwest of Yamen Glacier. The glacier drains southwards along the east slopes of Mount Ulmer and Mount Ojakangas, then turns southeast at Mount Washburn, flows east of Mount Cornwell and Mount Warren, and southwest of Branishte Peak, and together with Newcomer Glacier joins Rutford Ice Stream south of Foros Spur.

Crystal Glacier is in North Cascades National Park in the U.S. state of Washington, on the south slopes of Mount Shuksan. Descending from just east of the summit of Mount Shuksan, near its origination point, Crystal Glacier is connected to the larger Sulphide Glacier to the west. Crystal Glacier descends from , and is also connected to East Nooksack Glacier as well as Hanging Glacier near it uppermost margins. Both Crystal and Sulphide Glaciers have a series of high cascades which are collectively referred to as Sulphide Basin Falls.

In this Hubbard Glacier image from 16 July 2002, the glacier has closed off Russell Fjord from Disenchantment Bay. The waters behind the glacier rose in 10 weeks, creating a short lived Russell Lake. A glacial lake outburst flood is a type of outburst flood occurring when water dammed by a glacier or a moraine is released. A water body that is dammed by the front of a glacier is called a marginal lake, and a water body that is capped by the glacier is called a sub-glacial lake.

Topographic map of Smith Island. Vetrino Glacier (, ) is a 3.2 km long glacier on the northwest side of Imeon Range on Smith Island in the South Shetland Islands, Antarctica. It is situated northeast of Yablanitsa Glacier, southwest of Dalgopol Glacier and northwest of Ovech Glacier, drains the northwest slopes of Imeon Range north of Drinov Peak, northwest of Kostenets Saddle and west of Mount Pisgah, and flows northwestwards into Drake Passage both northeast and south of Gregory Point. The glacier is named after the town of Vetrino in northeastern Bulgaria.

The lower extent was marked by the Sandy Glacier Caves, possibly the largest glacier cave system in the lower 48 U.S. states. The glacier is a remnant of the massive glaciers that formed during the last ice age. It is bounded on the south by Yocum Ridge which also defines the northern side of Reid Glacier, and by a ridge on the north which defines part of the Hood River-Clackamas county border which also bounds the south side of Glisan Glacier. The glacier lies entirely within Mount Hood Wilderness.

Mammoth Glacier is in the Bridger Wilderness of Bridger-Teton National Forest, in the U.S. state of Wyoming. The glacier is on the west side of the Continental Divide which separates it from Dinwoody Glacier to the east. Mammoth Glacier is the largest glacier on the west side of the Continental Divide of the Wind River Range and occupies a large, north facing cirque on the north slopes of Twin Peaks and just west of Mount Woodrow Wilson. Mammoth Glacier is part of the largest grouping of glaciers in the American Rocky Mountains.

Simpson Glacier () is a glacier, 6 miles (10 km) long, in the Admiralty Mountains. It flows northward to the coast between Nelson Cliff and Mount Cherry-Garrard where it forms the Simpson Glacier Tongue. The latter feature was named by the British Antarctic Expedition, 1910–13, after Sir George Simpson, meteorologist of the expedition. The glacier described was mapped by United States Geological Survey (USGS), 1960–63,a and was so named by Advisory Committee on Antarctic Names (US-ACAN) because (with Fendley Glacier to the east) it nourishes the Simpson Glacier Tongue.

The glacier is bounded on the east by a slight rise shared with the Palmer Glacier (a popular skiing area north of Timberline Lodge since the 1930s) and on the northwest by Reid Glacier. It is the source of the Zigzag River which has eroded a large, steep canyon named Zigzag Canyon. Below the glacier, its snowfield varies significantly seasonally, varying in length by almost two miles (3.2 km). In 1922, a jökulhlaup originating from Zigzag Glacier as a flow of dark debris came out of a crevasse high on the glacier.

Grubb Glacier, pictured at center, is flanked by Mount Inverleith. Grubb Glacier () is a glacier flowing into Lester Cove, Andvord Bay, to the west of Bagshawe Glacier, on the west coast of Graham Land, Antarctica. The glacier appears on an Argentine government chart of 1952. It was named by the UK Antarctic Place-Names Committee in 1960 for Thomas Grubb, an Irish optician who designed and introduced the first aplanatic camera lens, in 1857.

Near by glaciers and river Dakshini Chamrao glacier, Balbala glacier and Paschimi Kamet glacier all the glacier drain their water in the Saraswati River which then joins Alaknanda River near Mana village one of the main tributaries of Ganga river. The River Dhauli Ganga emerges from Purbi Kamet Glacier and met Alaknanda river at Vishnu Prayag an 82 km journey from its mouth. Alaknanda river is one of the main tributaries of Ganga.

McLin Glacier () is a tributary glacier which flows north of McKenzie Nunatak into Graveson Glacier, in the Bowers Mountains of Antarctica. The glacier saddles with Carryer Glacier on the west and is nourished in part by Edlin Névé. It was named by the New Zealand Geological Survey Antarctic Expedition to this area, 1967–68, for Lieutenant Commander Robert D. McLin, U.S. Navy, a pilot of LC-130 Hercules aircraft in Antarctica that season.

This point is an important location to use in determining whether a glacier is growing or shrinking. A higher glacier equilibrium line will indicate that the glacier is shrinking, whereas a lower line will indicate that the glacier is growing. The terminus of a glacier advances or retreats based on the location of this equilibrium line. Scientists are using remote sensing to better estimate the locations of this line on glaciers around the world.

Sjogren Glacier Tongue () was a tongue of ice between wide, extending from Sjogren Glacier across Prince Gustav Channel toward Persson Island. Mapped from surveys by Falkland Islands Dependencies Survey (FIDS) (1960–61). The glacier tongue was an extension of the flow of Sjogren Glacier from which it took its name. As a result of glacier withdrawal, it has disappeared since at least 1994, with its area now covered by the Prince Gustav Channel.

Location of Pernik Peninsula on Loubet Coast, Antarctic Peninsula. Dabrava Glacier (, ) is the 14 km long and 4.5 km wide glacier on Pernik Peninsula, Loubet Coast in Graham Land, Antarctica, situated southwest of Murphy Glacier and north of Sölch Glacier. It drains the west slopes of Mount Deeley, flows northwestwards and enters Lallemand Fjord southwest of Orford Cliff. The glacier is named after the settlements of Dabrava in Northern, Northeastern, Southern and Southwestern Bulgaria.

Clarke Glacier is a 5 mile long glacier, which drains east to the coast of Victoria Land, immediately north of Lewandowski Point. The seaward extremity of this glacier merges with the flow of Davis Glacier and other glaciers from the south and contributes to the floating tongue of ice between Cape Reynolds and Lamplugh Island. The glacier was discovered and named by the British Imperial Antarctic Expedition (BrAE) (1907-1909) under Ernest Shackleton.

Bow Glacier is located in Banff National Park, Alberta, Canada, approximately northwest of Lake Louise. It can be viewed from the Icefields Parkway. Bow Glacier is an outflow glacier from the Wapta Icefield, which rests along the Continental Divide, and runoff from the glacier supplies water to Bow Lake and the Bow River. The glacier is credited for creating the Bow Valley before retreating at the end of the last glacial maximum.

The hotel was expanded in 1892 and 1904, and by 1907 the glacier was described as the "most visited glacier in the Americas". At this point, the glacier was called the "Great Glacier" by CPR promoters. The name "Illecillewaet" is an Okanagan First Nations word for "big water", and referred to the river before being applied to the glacier. It gradually replaced "Great" and was adopted by Parks Canada in the 1960s.

This glacier is situated to the west of the village of Khairkoot. The glacier is almost 2 km long in the lap of Sundur Top (3,660 m above sea level) Zaban Glacier is also the origin of Bachliri Nallaha, the main tributary of the Chenab River. Local tourists visit this glacier from March to mid-May. The glacier is connected by road to the Jammu-Srinagar National Highway, en route from Nowgam.

Erebus Glacier () is a glacier draining the lower southern slopes of Mount Erebus, Ross Island, Antarctica. It flows west to Erebus Bay where it forms the floating Erebus Glacier Tongue. It was named in association with Mount Erebus by the British National Antarctic Expedition, 1901–04, under Robert Falcon Scott. A large calving event took place on 1 March 1990, when a substantial portion of the Erebus glacier tongue was detached from the main glacier.

Zlatiya Glacier (, ) is the 6.7 km long and 3 km wide glacier on Brabant Island in the Palmer Archipelago, Antarctica situated north of Rush Glacier and west of upper Hippocrates Glacier. It drains west-southwestwards from Aluzore Gap, flows between Mount Sarnegor and Veles Bastion, and enters Dallmann Bay north of Sidell Spur and south of Fleming Point. The glacier is named after the settlements of Zlatiya in Northwestern and Northeastern Bulgaria.

It is surrounded by glaciers on both the sides Suralaya Glacier on the western side, sweta Bamak on the northern side, Both the glacier joins with Chaturangi Glacier and that later joins with Gangotri Glacier from there emerges the Bhagirathi River the main tributaries of river Ganga that later joins Alaknanda River the other main tributaries of river Ganga at Devprayag and became Ganga there after. The word "Bamak" is used for Glacier.

Vereyken Glacier () is a glacier in Victoria Land, Antarctica. Together with the Morning Glacier, it drains the northeast slopes of Mount Morning. Vereyken Glacier flows north between Riviera Ridge and Hurricane Ridge into Koettlitz Glacier. It was named by the Advisory Committee on Antarctic Names (US-ACAN) (1994) after Jill Vereyken, ASA manager of Field Support Services at McMurdo Station, who was active in coordination and planning of science support in Antarctica from 1984.

Lann Glacier () is a steep tributary glacier, long, in the north end of the Admiralty Mountains of Antarctica. The glacier is east of Rowles Glacier and flows northwest to enter Dennistoun Glacier. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–63, and was named by the Advisory Committee on Antarctic Names for Roy R. Lann, a U.S. Navy cook at Hallett Station, 1964.

Sigmen Glacier (, ) is a 2.2 km long and 2 km wide glacier draining the northwest slopes of Brugmann Mountains on Liège Island in the Palmer Archipelago, Antarctica. It is situated northeast of Zbelsurd Glacier and southwest of Shterna Glacier, draining the west-southwest slopes of Vazharov Peak and the northwest slopes of Mount Kozyak, and flows northwestwards to enter Palakariya Cove. The glacier is named after the settlement of Sigmen in southeastern Bulgaria.

Dimkov Glacier (, ) is a 6 km long and 4.3 km wide glacier draining the western slopes of Solvay Mountains on Brabant Island in the Palmer Archipelago, Antarctica. It is situated southwest of Rush Glacier and west of Jenner Glacier, and flows southwestwards between Kondolov Peak and Sheynovo Peak to enter Duperré Bay south of Humann Point. The glacier is named for the Bulgarian theoretician and practitioner of traditional medicine Petar Dimkov (1886-1981).

Ranges of steep rocks rise round the whole basin of this glacier, except in one or two places where they are interrupted by couloirs of snow. Finally, on the western side the mountain presents one gigantic face of rocky precipice. This face rises above the Weisshorn Glacier (Glacier du Weisshorn) and the Moming Glacier. The northern spur forks out at a considerable distance below the summit into two branches enclosing the Turtmann Glacier.

Eldridge Glacier is a major glacier in Denali National Park and Preserve in the U.S. state of Alaska. The long glacier originates on the east side of Explorers Peak, flowing northeast to a basin below Mount Eldridge, gathering flow from several glaciated cirques, then flowing southeast to the valley of the Chulitna River, where it gives rise to the Fountain River. A large unnamed tributary glacier joins Eldridge Glacier a few miles above its terminus.

Challenger Glacier is in North Cascades National Park in the U.S. state of Washington and is on the north slopes of Mount Challenger. Challenger Glacier descends from . Over wide, Challenger Glacier descends along a wide terminus with heavy crevassing and numerous icefalls, with a tongue of the glacier in the north descending to a proglacial lake. The ascent up Challenger Glacier is one of the most common routes to the summit of Mount Challenger.

Map of northern Sentinel Range. Vit Ice Piedmont (, ) is the glacier extending 12 km in north-south direction and 6 km in east-west direction in Sostra Heights on the east side of northern Sentinel Range in Ellsworth Mountains, Antarctica. It is situated north of the end of Embree Glacier, east of Bracken Peak, southwest of Anchialus Glacier and south of the end of Newcomer Glacier. The glacier flows eastwards into Rutford Ice Stream.

At some point the glacier reaches a pinning point where calving is reduced due to a fjord narrowing or shoaling and the glacier's AAR is near 100. This is occurring with LeConte Glacier and Yathse Glacier. Le Conte Glacier currently has an AAR of 90, is at a retracted position and seems likely to be set to advance after building a terminus shoal. The drop in calving rate allows the glacier to reestablish equilibrium.

Rusk Glacier is located on the eastern face of Mount Adams in the U.S. state of Washington. Starting at an elevation of over at just below The Castle, the glacier flows eastward down slope. A significant portion of the glacier is covered by rock debris and in the middle of the glacier, at about , there is a small ice-free island of rock. The glacier terminates at about at its rock- covered moraine.

Ice River Glacier is located northeast of Mount Olympus in the Olympic Mountains of Olympic National Park in the U.S. state of Washington. Starting at an elevation of on the northern slope of a subpeak of Mount Olympus known as Mercury (), the glacier flows northwest as it descends. The glacier reaches as low as before terminating. Though the glacier lies adjacent to the much larger Blue Glacier, an arête separates the two glaciers.

Over successive years, the limited amount of snow that falls on Vinson Massif compacts and is transformed into ice, forming glaciers. These glaciers follow the topography and flow down the mountain's valleys. The uppermost glacier occupies Jacobsen Valley on the north face of Mount Vinson, and flows either into Branscomb Glacier to the west or Crosswell Glacier to the east. The Crosswell Glacier flows into the Rutford Ice Stream via Ellen Glacier.

Lilliput Glacier is the smallest named glacier in the Sierra Nevada of California. The glacier has an area of , which is approximately 12.2 acres. In terms of area this is about the size of 48 typical suburb (100' x 100' or 1/4 acre) lots that single family home are built on. This glacier lies on the shaded north-facing vertical cliff of Mount Stewart, being the southernmost named glacier in the United States.

Marla Glacier (, ) is a glacier long and wide on the northeast side of Detroit Plateau on the southern Trinity Peninsula in Graham Land, Antarctica, situated south of Aitkenhead Glacier and north of Diplock Glacier. It is draining southeastwards along the east slopes of Povien Peak, then turning east between Mount Roberts and Bezenšek Spur, and flowing into Prince Gustav Channel in Weddell Sea. The glacier is named after Marla River in Northern Bulgaria.

Katsuk Glacier is in North Cascades National Park in the U.S. state of Washington, in a cirque to the north of Katsuk Peak and east of Kimtah Peak. Both Katsuk and Kimtah Peaks are prominent summits along a ridge known as Jagged Edge. Katsuk Glacier consists of three disconnected sections, the largest of which stretches for over in width. Kimtah Glacier is immediately west of Katsuk Glacier, while the Mesahchie Glacier lies to the east.

Hidden Creek Glacier is in North Cascades National Park in the U.S. state of Washington and is on the northwest slope of Hagan Mountain. Retreat of this glacier from 1979 to 2005 exposed several rock outcroppings in the middle of the glacier. The terminus of Hidden Creek Glacier only retreated between 1979 and 2011, however the increase in area of exposed rock outcroppings in the middle of the glacier indicates rapid thinning.

Dakshini Rishi Glacier on the eastern side and Trisul Glacier on the western side. both these glacier drains into Rish Ganga. Rishi Ganga met with Dhauli ganga near Rini. Later Dhauli ganga met with Alaknanda at Vishnu Pryag.

Gray Wolf Glacier is located in the US state of Montana. The glacier is situated in the Mission Mountains at an elevation of above sea level and is immediately northeast of Gray Wolf Peak. The glacier covers approximately .

Konowbreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It is located between Carlsfjella and Konowryggen, and debouches into St. Jonsfjorden. The length of the glacier is 12 kilometers. The glacier is named after Wollert Konow.

Penck Glacier () is a small glacier flowing northward along the west side of Bertrab Glacier to Vahsel Bay. Discovered by the German Antarctic Expedition, 1911–12, under Wilhelm Filchner, who named this feature for German geographer Albrecht Penck.

Blue Glacier is in the U.S. state of Washington. Blue Glacier is in Wenatchee National Forest and flows east from Gunsight Peak, descending from nearly . The much larger Chickamin Glacier is on the west side of Gunsight Peak.

Dakshini Rishi Glacier on the eastern side and Trisul Glacier on the western side. both these glacier drains into Rish Ganga. Rishi Ganga met with Dhauli ganga near Rini. Later Dhauli ganga met with Alaknanda at Vishnu Pryag.

It is part of the glacial divide between Nimitz Glacier and Rutford Ice Stream, overlooking Severinghaus Glacier to the southwest and Saltzman Glacier to the northeast. The col is named after the settlement of Karnare in Southern Bulgaria.

Surprise Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Alaska Range near Mount Dall, moving west. Its terminus is the source of the Tonzona River.

The Rotstock (3,699 m) is a mountain of the Bernese Alps, overlooking the Aletsch Glacier in the Swiss canton of Valais. It lies on the range between the Oberaletsch Glacier and the Aletsch Glacier, south of the Geisshorn.

View of the Rheinwaldhorn from the glacier The Paradies Glacier () is a 2.27 km long glacier (2007) situated in the Lepontine Alps in the canton of Graubünden in Switzerland. In 1973 it had an area of 3.99 km².

A broad unnamed glacier known colloquially as Snowking Glacier rests on the north face. Downslope of that glacier are Snowking Lake, Found Lake, and Cyclone Lake. Precipitation runoff from Snowking Mountain drains into tributaries of the Skagit River.

Edgeøyjøkulen is an ice cap glacier on Edgeøya, part of the Svalbard archipelago, Norway. The glacier covers and area of about .

The species name is derived from Latin glacialis (meaning glacier) and refers to the species occurrence in the Tibetan glacier area.

The area of the Oberaletsch Glacier, along with the Aletsch Glacier, was declared a UNESCO World Heritage Site in December 2001.

The U.S. Advisory Committee on Antarctic Names renamed the Warpasgiljo Glacier in Antarctica the Arthur Davis Glacier in honor of Davis.

The Rhine Glacier was a glacier during the last glacial period and was responsible for the formation of the Lake Constance.

Comparing images of the glacier taken in 1913 with those from 2009, indicates that the glacier has experienced thinning and retreat.

Gran Glacier () is a glacier in Antarctica that flows south into Mackay Glacier between Mount Gran and Mount Woolnough. It rises from a snow divide with Benson Glacier to the northeast. It was named after Mount Gran by the New Zealand Northern Survey Party of the Commonwealth Trans-Antarctic Expedition (1956–58), which visited the area in November 1957.

Sentinel Range map. Kopsis Glacier (, ) is a long and wide glacier on the east side of north-central Sentinel Range in Ellsworth Mountains, Antarctica that is draining northeastwards from Panicheri Gap, Voysil Peak and Mount Gozur to join Embree Glacier northwest of Mirovyane Peak. The glacier is named after the medieval town of Kopsis in Central Bulgaria.

RGO expedition to Spitzbergen: landing at Negribreen, 2014, watercolor on paper Negribreen is glacier at Spitsbergen, Svalbard. The glacier debouches into Storfjorden, in Olav V Land and Sabine Land, and forms a wide glacier front with the moving extreme point Kapp Antinori. The glacier covers an area of about . It is named after Italian geographer Christoforo Negri.

Aialik Glacier, a little over 15 miles from Seward, is the largest glacier in Aialik Bay, located in Kenai Fjords National Park. While fairly stable, the glacier calves most actively in May and June. A mural of two kayakers near the glacier painted by Byron Birdsall is at the office of the Kenai Fjords National Park.

Austerdalsbreen is a glacier in the municipality of Luster in Vestland, Norway. It is a side branch of the Jostedalsbreen glacier, and is included in the Jostedalsbreen National Park. The glacier is fed by the three steep glaciers Odinbreen, Torbreen and Lokebreen. The lower, flat part of the glacier displays a characteristic fishbone or lobster tail pattern.

Collier Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation generally above . Collier Glacier is on the west slopes of North Sister, an extinct shield volcano. Since its last maximum extent during the Little Ice Age (1350–1850 A.D.) the glacier has retreated over a mile.

The Exploradores Glacier is a glacier situated on the northeastern slope of Monte San Valentín, in the Aysén del General Carlos Ibáñez del Campo Region of Chile. The locality nearest to the glacier is Puerto Río Tranquilo, which is located on the western shore of General Carrera Lake. The glacier is part of Laguna San Rafael National Park.

Lekhziri Glacier () is a valley glacier located on the southern slopes of the Greater Caucasus Mountain Range in the Svaneti Region of Georgia. The length of the glacier is and its surface area is . The tongue of the glacier descends down to above sea level. Lekhziri consists of three separate glaciers; North, East and West Lekhziri.

During the winter and spring, Snowbird Glacier is often visited by backcountry skiers and snowmachiners. During the summer and fall, the glacier is frequented by hikers and backpackers. The glacier lies on the popular Bomber Traverse in the Talkeetna Mountains, which connects several remote mountain huts. A hiker stands above a massive moulin on Snowbird Glacier.

Location of Oscar II Coast on Antarctic Peninsula. Erden Glacier (, ) is the 6 km long and 2.8 km wide glacier on Oscar II Coast in Graham Land situated southwest of Lesicheri Glacier. It drains the southeast slopes of Forbidden Plateau, and flows southeastwards to join Jorum Glacier. The feature is named after the settlement of Erden in Northwestern Bulgaria.

Sennet Glacier () is a precipitous glacier between Yancey and Merrick Glaciers in the Britannia Range, flowing southward from Mount Aldrich to the Byrd Glacier. Named by Advisory Committee on Antarctic Names (US-ACAN), ACAN, in association with Byrd Glacier, for , submarine (Central Group of Task Force 68) of U.S. Navy Operation Highjump, 1946–1947, led by Admiral Byrd.

Meander Glacier () is a large meandering tributary to Mariner Glacier in Victoria Land, Antarctica. The glacier emerges in the vicinity of Mount Supernal and Hobbie Ridge and drains generally eastward for through the Mountaineer Range to join Mariner Glacier just east of Engberg Bluff. The descriptive name was given by the New Zealand Geological Survey Antarctic Expedition, 1962–63.

Teton Glacier is a mountain glacier located below the north face of Grand Teton in Grand Teton National Park, Wyoming, United States. Its neighbors are Mount Owen to the west and Teewinot Mountain to the north. Teton Glacier is the largest of the twelve named glaciers in the park. In 1971, the glacier was approximately long and wide.

The Yakutat Glacier is a glacier in the Brabazon Range of southeastern Alaska. It is one of the fastest moving glaciers in the world, and has been retreating since Little Ice Age.Retreat of Yakutat Glacier August 21, 2014 by Adam Voiland, NASAYakutat Glacier Rapid Retreat, Alaska by Mauri Pelto December 5, 2009 Approximate elevation 1,010 feet (308 meters).

Lathrop Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation generally above on the steep northeast slope of Mount Thielsen, an extinct shield volcano. Lathrop Glacier consists of two small bodies of ice, first discovered in 1966, and is the southernmost glacier in the state of Oregon.

Diobsud Creek Glacier is in North Cascades National Park in the U.S. state of Washington and is on the east slopes of Bacon Peak. Diobsud Creek Glacier has a shallow gradient, descending to the east from for a distance of nearly . The ridge is an arête which separates Diobsud Creek Glacier from Green Lake Glacier to the north.

Shterna Glacier (, ) is the glacier extending 3.6 km in east-west direction and 2.2 km in north-south direction on Liège Island in the Palmer Archipelago, Antarctica. It is situated northeast of Sigmen Glacier, draining the north slopes of Brugmann Mountains and flowing northwards into Boisguehenneuc Bay. The glacier is named after the settlement of Shterna in Southern Bulgaria.

The Belvedere Glacier () is a valley glacier located above Macugnaga of the Valle Anzasca in the region of Piedmont. The glacier lies at the base of the east face of Monte Rosa. It reaches approximately above sea level at its highest point and terminates near the Alpe Burki at about . The glacier is mostly covered by rocks.

This eventually persuaded Rusk, but years later when he wrote Tales, Rusk repeated his wish that the glacier be known as Reid Glacier. Rusk also recommended that the Lyman Glacier be named as such in honor of William Denison Lyman, who had done some to the first research into Adams. Reid officially named Rusk Glacier after him.

Hileman's 1938 image of Grinnell Glacier Hileman's 1938 photo of Grinnell Glacier has been used as an early image documenting the state of that glacier in the first half of the 1900s. Subsequent photos in the ensuing decades, which have been taken from the same vantage point, show evidence of a steady state of retreat for that glacier.

Schweitzer Glacier (, ) is a glacier which drains west along the north side of Littlewood Nunataks into Vahsel Bay. The Lerchenfeld Glacier, trending west- northwestward, coalesces with the lower portion of this glacier. Discovered by the German Antarctic Expedition, 1911–12, under Wilhelm Filchner. He named it for Major Schweitzer, first president of the German Antarctic Expedition Society.

Grinnell Lake is located in Glacier National Park, in the U. S. state of Montana. Named after George Bird Grinnell, the lake has an opaque turquoise appearance from the rock flour (silt) which is transported to the lake from Grinnell Glacier. Grinnell Lake is accessible via the Grinnell Glacier Trail and is from the Many Glacier Hotel.

Albrecht Penck Glacier () is a glacier between the Fry Glacier and the Evans Piedmont Glacier, draining northeast toward Tripp Bay on the coast of Victoria Land, Antarctica. It was first charted by the British Antarctic Expedition (1907-09) which named this feature for Albrecht Penck, the Director of the Institute of Oceanography and of the Geographical Institute in Berlin.

The Scott Glacier is a major glacier, long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, with the Amundsen Glacier to the west and the Leverett and Reedy glaciers to the east.

Peters Glacier is a glacier in the Arctic National Wildlife Refuge in the U.S. state of Alaska. The glacier is on the west side of Mount Chamberlin, one of the tallest mountains in the eastern end of the Brooks Range. The glacier was named in 1959 by the U.S. Air Force Cambridge Research Center for nearby Lake Peters.

Fluvio refers to things related to rivers and glacial refers to something that is of ice. Fluvio-glacial refers to the meltwater created when a glacier melts. Fluvio-glacial processes can occur on the surface and within the glacier. The deposits that happen within the glacier are revealed after the entire glacier melts or partially retreats.

The glacier was, at that time, a glacier that nearly reached tidewater.(Wilderness Essays, The Alaska Trip (pg 60) John Muir). It has since receded into the mountains, becoming a valley glacier, and created its very own glacial lake in the glacier's moraine (similar to the Mendenhall Glacier and lake) about one mile inland from the Chilkat Inlet.

Davenport Glacier is located in a cirque to the southeast of Boston Peak, North Cascades National Park in the U.S. state of Washington. The glacier is approximately in length resting at between . The glacier is also northeast of Sahale Mountain and separated from the much larger Boston Glacier to the north by an arête called "Ripsaw Ridge".

Meade Glacier is located in the Goat Rocks region in the U.S. state of Washington. The glacier is within the Goat Rocks Wilderness of Snoqualmie National Forest, south of Conrad Glacier and immediately east of Gilbert Peak. Meade Glacier is split into three sections and the lower ablation zone at is not connected to the upper accumulation zone at .

The Rathong Glacier is an important glacier of Western Sikkim, India. The source of the Rathong River flows from the snout of Rathong Glacier. This glacier extends from Rathong La in the north almost to the top of Chowrikiang Valley in the South. It is fed by the Mt. Rathong (6678m) and Ice Falls of Kabru group of peaks.

Silk Glacier () is a glacier, 10 miles (16 km) long, draining the east slopes of the Churchill Mountains between Mount Frost and Mount Zinkovich to enter Nursery Glacier. Named by Advisory Committee on Antarctic Names (US-ACAN) for Cdt. P.R.H. Silk, RNZN, commanding officer of HMNZS Endeavour II in Antarctic waters, 1963–64.Silk Glacier Geographic Names Information System.

The Rongbuk Glacier () is located in the Himalaya of southern Tibet. Two large tributary glaciers, the East Rongbuk Glacier and the West Rongbuk Glacier, flow into the main Rongbuk Glacier. It flows north and forms the Rongbuk Valley north of Mount Everest. The famous Rongbuk Monastery is located at the northern end of the Rongbuk valley.

Price Glacier is in North Cascades National Park in the U.S. state of Washington, on the northeast slopes of Mount Shuksan, below the subpeak known as Nooksack Tower. Price Glacier descends from and is the steepest and most heavily crevasseed glacier on Mount Shuksan. The disconnected lowest portions of Price Glacier calve small icebergs into Price Lake.

Sulphide Glacier is in North Cascades National Park in the U.S. state of Washington, on the south slopes of Mount Shuksan. Descending from the summit tower of Mount Shuksan, it is connected to Crystal Glacier to the east. Sulphide Glacier descends from . Sulphide Glacier is along the route taken when Mount Shuksan was first climbed in 1906.

Map of Glacier Bay. Red lines show glacial terminus positions and dates during retreat of the Little Ice Age glacier. Maps showing retreat of Muir Glacier from 1941 to 1982 There are thousands of glaciers in Alaska but only few have been named. The Columbia Glacier near Valdez in Prince William Sound has retreated in the last 25 years.

Harbardsbreen is the 10th largest glacier in mainland Norway. It is located on the south side of the Tverrådalskyrkja mountain in the Breheimen mountain range in the municipality of Luster in Vestland county, Norway. The glacier is inside Breheimen National Park, just northeast of the Spørteggbreen glacier. The village of Skjolden lies south of the glacier.

Anderson Glacier was a glacier located in a cirque south of Mount Anderson in the Olympic Mountains and Olympic National Park. The southward-facing glacier starts on the steep headwalls of the cirque at about to . It flows down to about before terminating. Meltwater from the glacier enters a lake at about before tumbling down a steep cliff.

Eiger Glacier The Eiger Glacier () is a glacier situated on the north-west side of the Eiger in the Bernese Alps of Switzerland. The glacier is within the municipality of Lauterbrunnen in the canton of Bern. In 1973 it had an area of , and a length of . By 2005 its length had reduced to 2.5 km.

Double Glacier is an long glacier in the Kenai Peninsula Borough of Alaska, located west-northwest of Kenai. As its name suggests, Double Glacier is divided into two lobes. An unnamed lava dome complex of Pleistocene age forms a nunatak in Double Glacier. K–Ar dating of the complex indicates that it formed 627,000 to 887,000 years ago.

Detail view of the glacier. The Aialik Glacier is a glacier in the Kenai Peninsula Borough of Alaska. It drains into Aialik Bay. Part of Kenai Fjords National Park, it (along with many other glaciers) drains the Harding Icefield.

Grinnell Falls is a waterfall in Glacier National Park, Montana, US. Grinnell Falls have several major drops in its descent from Grinnell Glacier with the highest estimated at . The falls are in the Many Glacier region of the park.

Dakshini Rishi Glacier on the eastern side and Trisul Glacier on the western side. both these glacier drains into Rishi Ganga. Rishi Ganga met with Dhauli ganga near Rini. Later Dhauli ganga met with Alaknanda river at Vishnu Prayag.

Mount Jackson as viewed from the summit Mount Siyeh, another of Glacier National Park's 10,000 foot peaks. Jackson Glacier lies directly to the left of the mountain. Mountains in Glacier National Park (U.S.) are part of the Rocky Mountains.

Dachstein Glacier is a glacier located above the town of Ramsau am Dachstein in Austria. Snow is at the top of the glacier throughout the year. However snow is soft in summer. This mountain is located south of Salzburg.

At the head of Amalia Fjord is Amalia Glacier. El Brujo Glacier is found in Asia Fjord, which is another glacier spilling from the Southern Patagonian Ice Field. Calvo Fjord splits into several arms towards which also descend glaciers.

Glacial Lake at the base of Saint Mary's Glacier Saint Mary's Glacier (or Saint Marys) is a semi-permanent snowfield located in Arapaho National Forest in the U.S. state of Colorado. Saint Mary's Glacier is southeast of James Peak.

The glacier ranges in elevation from at the foot of the steep cliff to at the moraine. One arm of the glacier extends south down to . Between 1904 and 2006, Crescent Glacier lost 6 percent of its surface area.

The glacier was so named by the FIDS because a sledge dog was rescued from a grotto-like crevasse in the glacier.

Hooker Glacier is located in Shoshone National Forest, in the U.S. state of Wyoming, WNW of Mount Hooker. The glacier descends from .

Heim Glacier (), is a glacier in eastern Greenland. It is named after Swiss geologist and glacial phenomena expert Albert Heim (1849–1937).

On the northern side of Piz Nair lies a small glacier, the Fellelifirn. Large lateral moraines can be seen below the glacier.

The Silverthrone Glacier is a glacier at the northwest head of Knight Inlet in southwestern British Columbia, Canada (51°26'00N, 125°53'00W).

Vicha Glacier. SCAR Composite Gazetteer of Antarctica The glacier is named after the ancient and medieval fortress of Vicha in Northeastern Bulgaria.

Archer Glacier () is a glacier flowing northwest into the head of Bolson Cove, Flandres Bay, on the west coast of Graham Land.

Sandy Glacier decreased in area by 40% between 1907 and 2004. The glacier terminus has retreated by over the same time period.

This NASA image showing glacier velocities on the Lambert Glacier has a box location of the area shown in the other photograph The glacier is important in the study of climate change because very small changes in the climate can have significant consequences for the flow of ice down the glacier. Most studies of the Lambert Glacier are done with remote sensing due to the harsh conditions in the area. The photo reproduced here (above) shows a small tributary right-flank glacier flowing down from the ice-covered East Antarctic Plateau, flanked by slower-moving ice flowing down over a steep escarpment. The ice-fall which so impressively illustrates the flow characteristics of glacier ice is only about 6 km wide, and Lambert Glacier proper is off the bottom right corner of the photo.

Huron Glacier from Camp Academia, with Moon Bay, Half Moon Island and Greenwich Island in the background. Upper Huron Glacier from Ongal Peak, with Kuzman Knoll and Bowles Ridge in the background. Huron Glacier is a } long and wide glacial flow on Livingston Island in the South Shetland Islands of Antarctica, situated east of Perunika Glacier, southeast of Kaliakra Glacier, south of Struma Glacier, west-northwest of Iskar Glacier and northeast of Huntress Glacier. It is bounded by Bowles Ridge to the north, Wörner Gap to the west and the Tangra Mountains to the south, receiving ice influx from several tributary glaciers draining the mountain's northern slopes between Mount Friesland and Helmet Peak, and running east-northeastwards to empty into Moon Bay south of Elemag Point and north of Yana Point.

Filchner named the feature for Kaiser Wilhelm, but the Emperor requested it be named for its discoverer. The shelf is nourished primarily by the Slessor Glacier, the Recovery Glacier, and the Support Force Glacier, all located east of Berkner Island.

Foolsmate Glacier () is a small, heavily crevassed tributary glacier flowing northeast to enter Priestley Glacier, west of Shafer Peak, in Victoria Land, Antarctica. The name was applied by the Southern Party of the New Zealand Geological Survey Antarctic Expedition, 1962–63.

Timpanogos Glacier is a rock glacier located on Mount Timpanogos in the Wasatch Range within the Mount Timpanogos Wilderness (in the Uinta-Wasatch- Cache National Forest) in northeastern Utah County, Utah, United States, and is the last known glacier in Utah.

Associated with it is the Zélée Glacier Tongue (), a glacier tongue about wide and long which extends seaward from Zélée Glacier. Delineated from air photos taken by U.S. Navy Operation Highjump, 1946–47, and named for the French corvette Zélée.

On the east side of the Affliction Glacier, rhyodacite of the Job Assemblage overlies porphyritic andesite of the older Pylon Assemblage. The more recently formed Capricorn Assemblage overlies the Job Assemblage at the head of Affiction Glacier and Capricorn Glacier.

Mount Logan () is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Logan Glacier is immediately north of Mount Logan and Red Eagle Glacier lies to the east. Mount Logan is situated along the Continental Divide.

The Richardson Glacier lies to the southeast of the summit, with the Pilz Glacier and Butterfly Glacier stretching across the northern slope. Precipitation runoff from the peak drains into the White River and Napeequa River, both tributaries of the Wenatchee River.

Swamp-like canal areas and streams underlie the glacier. The upstream swamp canals feed streams with dry areas between the streams which retard flow of the glacier. Due to this friction the glacier is considered stable in the short term.

Buckskin Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier originates on the east side of The Moose's Tooth, flowing east, then southeast, for before giving rise to the Hidden River.

Cantwell Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The long glacier originates from the crest of the Alaska Range in the eastern part of the park, giving rise to Cantwell Creek.

Penny Royal Glacier sits in the Talkeetna Mountains in an undeveloped wilderness area, at an elevation between approximately 4,600-6,000 ft. Penny Royal is an alpine glacier surrounded by mountains, cliffs, and glacial valleys. The glacier can receive snowfall year- round.

Between 1927 and 2009, Anderson Glacier lost more than 90 percent of its surface area. By 2011, the glacier was gone. The lack of glacial meltwater from the Anderson Glacier has caused the Quinault River to reach new recorded lows.

Link Sar is located in the Masherbrum range of the Karakoram between the head of the Charakusa Glacier and the Kaberi Glacier. The peak lies on a horseshoe which links K6 and K7 around the head of the Charakusa Glacier.

Antoniabreen is a glacier in Wedel Jarlsberg Land at Spitsbergen, Svalbard. The glacier has a length of about twelve kilometers and a width of two kilometers, and is located east of Martinfjella. The glacier is named after Maria Antonia of Parma.

Linked by a saddle to Casanovas Peak in the west, and surmounting Berkovitsa Glacier to the northwest, Tundzha Glacier to the east and Verila Glacier to the southwest. The feature was charted and named descriptively by Discovery Investigations personnel in 1935.

Glacier movement is resisted by debris, whether it is inside the glacier or under the glacier. This can affect the amount of movement that is made by the glacier by a large percentage especially if the slope on which it lies is low. The traction caused by this sediment can halt a steadily moving glacier if it interferes with the underlying sediment or water that was helping to carry it. The Great Lakes were created due to basal movement.

Ferguson Glacier () is a glacier on the east side of Gallagher Ridge in the Asgard Range, McMurdo Dry Valleys, Antarctica. It flows north parallel to Decker Glacier, the two glaciers merging before reaching the snout of Wright Lower Glacier. In association with Tractor Corner nearby, it was named by the New Zealand Geographic Board in 1998 to recall the passage of Massey Ferguson tractors over the Wright Lower Glacier en route to Wright Valley in 1967.

Miller Glacier is a glacier about wide, described by Griffith Taylor as a transection glacier lying in a transverse trough and connecting Cotton Glacier and Debenham Glacier in Victoria Land, Antarctica. It was discovered by the Western Geological Party, led by Taylor, of the British Antarctic Expedition, 1910–13, and was named by Taylor for M.J. Miller, Mayor of Lyttelton, and the shipwright who repaired the expedition vessel, Terra Nova, prior to its voyage from New Zealand.

Howchin Glacier () is a glacier between Ward Glacier and Walcott Glacier, on the east side of the Royal Society Range in Victoria Land, Antarctica. Brandau Crater is an ice-free volcanic crater lying to the south of the snout of Howchin Glacier on Chancellor Ridge, Royal Society Range It was discovered by a party led by Thomas Griffith Taylor of the British Antarctic Expedition, 1910–13, and named for Professor W. Howchin, a geologist of Adelaide.

The McBride Glacier is the only tidewater glacier in the eastern arm at a distance of from Bartlett Cove. Of the other glaciers on the western arm, Johns Hopkins Glacier is at the farthest end – from the entrance to the bay while the Margerie Glacier is about away. The National Park Service manages a total of of marine waters of the Glacier Bay. It covers a coastline of including some reach of the coast outside the Bay.

Lewis Glacier is in the U.S. state of Oregon. The glacier is situated in the Cascade Range at an elevation generally above . Lewis Glacier is on the southeast slopes of South Sister, an inactive stratovolcano. Since its last maximum extent during the Little Ice Age (1350–1850 A.D.) where it descended to an elevation of , the glacier has been in a general state of retreat and the terminus of the glacier was reported in 2005 to be at approximately .

Sentinel Range map Razboyna Glacier (, ) is the long and wide glacier in Petvar Heights on the southeast side of Sentinel Range in Ellsworth Mountains, Antarctica situated north of Drama Glacier, east of Kornicker Glacier, and south of the lower course of Thomas Glacier. It is draining the north slopes of Bagra Peak, and flowing northeastwards to leave the range north of Long Peak. The feature is named after the settlements of Razboyna in northeastern and southeastern Bulgaria.

Location of Nordenskjöld Coast. Zlokuchene Glacier (, ) is the 13 km long and 3.5 km wide glacier on Nordenskjöld Coast in Graham Land, Antarctica situated north of Risimina Glacier, east of Rogosh Glacier and south of the lower course of Drygalski Glacier. It is draining from Mrahori Saddle eastwards between Kyustendil Ridge and Lovech Heights to flow into Weddell Sea northwest of Pedersen Nunatak. The feature is named after the settlements of Zlokuchene in western and southern Bulgaria.

Glacier National Park was established in 1910, immediately north of the main line of the Great Northern Railway. The railroad immediately began a massive concession development program in and near the park, which included the construction of two major hotels and nine smaller "chalet" complexes. The cornerstone of the project was Glacier Park Hotel (now Glacier Park Lodge), located just outside the park boundary at Glacier Park Station (East Glacier). The hotel had a capacity of 400 guests.

Rusk climbed Glacier Peak in August 1906 with A. L. Cool. They were the third party to climb Glacier Peak and the first to climb the east side. The day before the climb, Rusk named Cool Glacier after Cool as he was the first person to set foot on it. The day after the climb, while they were exploring the lower slopes of Glacier Peak, Rusk named Chocolate Glacier after the chocolate colored water the emanated from it.

Location of Hemimont Plateau on the Antarctic Peninsula. Renaud Glacier () is a heavily crevassed glacier on the east side of Hemimont Plateau flowing southeast to enter Seligman Inlet between Lewis Glacier and Choyce Point, on the east coast of Graham Land. The glacier was first photographed by the United States Antarctic Service (USAS), 1939–41. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Andre Renaud, Swiss glaciologist and chairman of the Swiss Glacier Commission, 1955–74.

Fox Glacier / Te Moeka o Tuawe is a temperate maritime glacier located in Westland Tai Poutini National Park on the West Coast of New Zealand's South Island. Like nearby Franz Josef Glacier, Fox Glacier is one of the most accessible glaciers in the world, with a terminal face as low as 300 m above sea level, close to Fox Glacier village / Weheka. It is a major tourist attraction and about 1000 people daily visit it during high tourist season.

Kleptuza Glacier (, ) is a 6 km long and 6 km wide glacier draining the east slopes of Mount Hector in the Trojan Range and the north slopes of Osterrieth Range on Anvers Island in the Palmer Archipelago, Antarctica. Situated southeast of Thamyris Glacier and west of Altimir Glacier. Flowing northwards to enter Fournier Bay east of Madzharovo Point and west of Studena Point. The glacier is named after the karst spring of Kleptuza in southern Bulgaria.

Sentinel Range map Patleyna Glacier (, ) is the long and wide glacier on the east side of north-central Sentinel Range in Ellsworth Mountains, Antarctica, situated north of the upper course of Ellen Glacier. It is draining the east slopes of Mount Todd and the north slopes of Chepino Saddle, and flowing north-northwestwards to join Embree Glacier southeast of Mount Goldthwait and west of Oreshak Peak. The glacier is named after the nature reserve of Patleyna in Northeastern Bulgaria.

In a paper published in 2009 by the University of Zurich, the Swiss glacier survey of 89 glaciers found 76 retreating, 5 stationary and 8 advancing from where they had been in 1973. The Trift Glacier had the greatest recorded retreat, losing of its length between the years 2003 and 2005. The Grosser Aletsch Glacier is the largest glacier in Switzerland and has been studied since the late 19th century. Aletsch Glacier retreated from 1880 to 2009.

The Puyallup Glacier is a glacier on the west flank of Mount Rainier in Washington. It covers and contains 10.2 billion ft3 (289 million m3) of ice. Sharing the same source of ice as the northern South Mowich Glacier, the Puyallup Glacier begins as a branch off the ice stream that flow out of the Sunset Amphitheater. From the split at around , the glacier expands into a broad sheet of ice ranging from to in elevation.

Due to orographic lift and the glacier's proximity to the Pacific Ocean, more precipitation falls on the Blue Glacier than any other glacier in the lower 48 United States. About of precipitation falls on the upper reaches of Mount Olympus and Blue Glacier each year. During winter, most of the precipitation on Blue Glacier consists of snow. In addition, a significant amount of rain falls on the Blue Glacier as well, especially during spring and summer.

It was first surveyed by the Falkland Islands Dependencies Survey in 1946–47, and named "East Balch Glacier". With "West Balch Glacier" it was reported to fill a transverse depression across Graham Land, but further survey in 1957 showed that there is no close topographical alignment between the two. The name "Balch", for Edwin S. Balch, an American Antarctic historian, has been limited to this glacier and an entirely new name, Drummond Glacier, approved for the west glacier.

Observations in 2005 suggest that the lowest thousand feet or several hundred meters of the glacier is stagnant and will likely disappear. In the pictures, this section of the glacier is gray with rock debris and has few crevasses. On the west side of Boulder Creek is a small waterfall revealed by the recent recession of the glacier. Stagnant, rock-debris-covered glacier terminus in 2004 Boulder Glacier may be approached via the Boulder Ridge Trail number 605.

Grasshopper Glacier is located in Shoshone National Forest, in the US state of Wyoming on the east of the Continental Divide in the Wind River Range. Grasshopper Glacier is in the Fitzpatrick Wilderness, and is part of the largest grouping of glaciers in the American Rocky Mountains. The glacier flows north, and glacial runoff supplies water to Grasshopper Creek, flowing eventually into the Wind River. The glacier shares a glacial margin with Klondike Glacier, located to the south.

Location of Nordenskjöld Coast. Darvari Glacier (, ) is the 9 km long in northwest-southeast direction and 1.7 km wide glacier on Nordenskjöld Coast in Graham Land, Antarctica situated southwest of Boryana Glacier and northeast of Zaychar Glacier. It drains the southeast slopes of Detroit Plateau, flowing between Rice Bastion and Grivitsa Ridge, and entering Mundraga Bay in Weddell Sea 6 km north of Fothergill Point. The glacier is named after the settlement of Darvari in Northern Bulgaria.

Grasshopper Glacier is in the Beartooth Mountains, Custer National Forest, Montana, U.S. The glacier is within the Absaroka-Beartooth Wilderness, a part of the Greater Yellowstone Ecosystem. Grasshopper Glacier is approximately long and wide. Starting at a point more than above sea level, the glacier originally was more than long but has receded significantly since first researched in the early 20th century. As of 2007, the glacier consists of several smaller glaciers, each occupying a different north-facing cirque.

The Lindbergh Range is an up to 3,171 m high cluster of nunataks, some of which are extensive ridges rising above the ice. It is located west of the Christian IV Glacier and east of the Upper Frederiksborg Glacier (Øvre Frederiksborg Gletscher), an ice cap west of which lie the Frederiksborg Nunataks, located north of the Frederiksborg Glacier. The Isfald Glacier is a smaller glacier located at the southern end. The vast Greenland Ice Sheet lies to the northwest.

Taylor Glacier, Taylor Valley and Blood Falls, 2013 The Taylor Glacier is an Antarctic glacier about long, flowing from the plateau of Victoria Land into the western end of Taylor Valley, north of the Kukri Hills, south of the Asgard Range. The middle part of the glacier is bounded on the north by the Inland Forts and on the south by Beacon Valley. The glacier was discovered by the British National Antarctic Expedition (1901–04) and at that time thought to be a part of Ferrar Glacier. The Western Journey Party of the British Antarctic Expedition 1910 determined that the upper and lower portions of what was then known as Ferrar Glacier are apposed, i.e.

In the late 1970s, Lynch Glacier extended into Pea Soup Lake; however, repeat photography indicates the glacier has since retreated above the lake.

Gyrfalcon Lake is located in Glacier National Park, in the U. S. state of Montana. Gyrfalcon Lake is east of Two Ocean Glacier.

The flow of water in the river has been decreasing in recent years as the source glacier (Kailash Kund glacier) has been retreating.

Meridian Glacier () is a broad glacier, long, which flows south along the west side of Godfrey Upland and joins Clarke Glacier between Behaim Peak and Elton Hill, in southern Graham Land, Antarctica. Finn Ronne and Carl R. Eklund of the United States Antarctic Service travelled along this glacier in January 1941. It was photographed from the air by the Ronne Antarctic Research Expedition in November 1947, and was surveyed by the Falkland Islands Dependencies Survey in December 1958. The glacier was so named by the UK Antarctic Place-Names Committee because the glacier flows from north to south along the meridian.

It is surrounded by Glaciers on the eastern side of the Janhukut is Satopanth Bamak (Glacier),on the western side its Maiandi Bamak (Glacier) On the southern side Gangotri glacier and on the Northern side Bhagirathi kharak Glacier. From the Maiandi Bamak and Gangotri glacier emerges Bhagirathi river and on the other side Satopanth Bamak and Bhagirathi kharak glacier,emerges Alaknanda river two main tributaries of Ganga. These two river meets at Devpryag from their starts the name Ganga. The entire surrounding area are protected within the Gangotri National Park, the largest conservation area in India.

Emerald Lake and the Timpanogos Glacier from the summit of Mount Timpanogos, September 2014 The glacier is situated on the north slope of Mount Timpanogos (). The best evidence indicates that the Timpanogos Glacier was once a "true" glacier with crevasses present in the early 20th century, but that the surface portion was lost during the dust bowl drought of the 1930s and reduced to a permanent snowfield. The glacier is considered to be a rock glacier, since the remaining ice is buried in the talus. However, in 1994 the rocks parted, revealing a crevasse or meltwater channel in the buried ice.

Scudding Glacier () is an abrupt glacier, 3 nautical miles (6 km) long, descending into the end of Alatna Valley from the south side of Mount Gunn in the Convoy Range, Victoria Land. This high elevation glacier is adjacent to the neve of Cambridge Glacier and snow laden katabatic winds make their first descent into Alatna Valley over the glacier. Even on days of relatively light winds, snow clouds derived from the high neve may be seen swirling and scudding down this glacier. So named by the 1989-90 New Zealand Antarctic Research Program (NZARP) field party to the area.

Nugget Falls, also known as Nugget Creek Falls or Mendenhall Glacier Falls, is a waterfall downstream of the Nugget Glacier, at the base of Bullard Mountain, in the U.S. state of Alaska. Formed by the creek from the Nugget Glacier, the waterfall drops in two tiers of and onto a sandbar in Mendenhall Lake, which is the freshwater pool at the face of the Mendenhall glacier. The lake then drains via Mendenhall River into the Inside Passage. The waterfall is fed by Nugget Creek, which is in turn fed by the Nugget Glacier, a tributary glacier on the mountainside east of Auke Bay.

The Coalman Glacier (also Coleman Glacier) is a glacier located on the upper slopes of Mount Hood in the U.S. state of Oregon. It is the mountain's highest glacier ranging from about , located within the crater rim, southwest of the peak. It was named for Elija Coalman (variously spelled Elijah Coleman), an early mountain guide who climbed Mount Hood 586 times. citing A group of climbers from The Mazamas ascend Mount Hood's Hogsback summer 1963 Coalman Glacier is the second most frequently visited glacier on the mountain because it is part of the popular South Climbing route from Timberline Lodge.

On the Glacier Noir, with the Montagne des Agneaux (background) The glacier may be easily reached on foot from the hut of Refuge Cézanne at the Pré de Madame Carle, where the road from the climber's village of Ailefroide ends in the Vallouise at a large car park. Initially following the path to the Refuge du Glacier Blanc, it bears left where the paths fork and reaches the lateral moraine of the glacier on which there is a route high above the glacier on that side.Walk 6013 - Pré de Madame Carle - Glacier Noir, Ecrins NP at www.walkingeurope.info. Accessed on 19 Dec 2010.

Honeycomb Glacier is located in the Glacier Peak Wilderness in the U.S. state of Washington. The glacier is mainly in Mount Baker-Snoqualmie National Forest, but a small segment near the top of the glacier extends into Wenatchee National Forest. Honeycomb Glacier is nearly connected to White River and Suiattle Glaciers and is separated from them by an arête off the Kololo Peaks. Honeycomb Glacier is one of the largest glaciers found in the North Cascades, but since the end of the Little Ice Age (around the year 1850), retreated between then and the year 2005.

The glacier has decreased in surface area by 47% between 1904 and 2006. In 1901, when Mount Adams was being mapped and its glaciers named by Harry Fielding Reid, Reid's companion and guide, Claude Ewing Rusk, wanted to name the glacier Reid Glacier in honor of Reid; however, Reid insisted that it should be named something else because he thought it improper to place his own name on the map that he was making and the Mazamas were trying to name a glacier on Mount Hood after him. This eventually persuaded Rusk and he conceded to name the glacier Adams Glacier.

Suiattle Glacier is located in the Glacier Peak Wilderness in the U.S. state of Washington. The glacier is within Mount Baker-Snoqualmie National Forest and nearly touches Honeycomb and White River glaciers separated from them by an arête off the Kololo Peaks at its uppermost reaches. Suiattle Glacier has retreated significantly since the end of the Little Ice Age, and from approximately the years 1850 to 1924 lost of its length. Between 1924 and 1940, the glacier retreated an additional , then during a cooler and wetter period between 1967 and 1979, the glacier had a small advance of .

Many of these glacier caves were big enough to explore, like the glacier caves on the summit of Mount Rainier. Most of the glacier caves were located near the 1980s lava dome, where hot steam and volcanic gas emissions from hidden fumaroles on the crater floor or lava dome melted holes in the young glacial ice. About 7,900 feet or 2.4 km of caves and passageways in the glacier were mapped and studied. ;Other glaciers and new rock glaciers Since 2004, new glaciers have formed on the crater wall above Crater Glacier feeding rock and ice to Crater Glacier below.

Benson Glacier () is a glacier about long, draining the eastern part of Flight Deck Neve and continuing east between Fry Glacier and Mackay Glacier into the northern part of Granite Harbour where it forms a floating tongue. It was mapped in 1957 by the New Zealand Northern Survey Party of the Commonwealth Trans-Antarctic Expedition (1956–58), and indicated as a somewhat longer glacier including the present Midship Glacier. It was named by the party after W.N. Benson, formerly professor of geology at the University of Otago, New Zealand, whose publications include a major contribution to the petrology of Victoria Land.

Peters Glacier, also known as Hanna Glacier and Hudeetsedle Toyaane' is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier runs from the Peters Basin icefield in a deep valley to the north of Denali's Wickersham Wall, between Denali and Peters Dome, falling from the icefield via the Tluna Icefall, where it is joined by Jeffery Glacier. It exits the Alaska Range to the north, forming the source of the Muddy River. Peters Glacier was named by A.H. Brooks for U.S. Geological Survey topographer William John Peters, who surveyed in Alaska from 1898 to 1902.

The Volta Glacier is located in Mount Aspiring National Park in the Southern Alps of the South Island of New Zealand. It is split into upper and lower glaciers which are connected by an icefall. The Upper Volta Glacier is between in altitude and is surrounded by the 3 peaks of Glacier Dome, Pickelhaube and Fastness Peak, while the Lower Volta Glacier sits directly under the North side of Mount Aspiring / Tititea and lies between . The Lower Volta Glacier feeds an unnamed lake at the Glacier Toe, which in turn feeds the Waiatoto River which eventually runs out to the West Coast.

A glacial terminus Satellite view of changing glacier termini in the Bhutan- Himalaya. A glacier terminus, toe, or snout, is the end of a glacier at any given point in time. Although glaciers seem motionless to the observer, in reality glaciers are in endless motion and the glacier terminus is always either advancing or retreating. The location of the terminus is often directly related to glacier mass balance, which is based on the amount of snowfall which occurs in the accumulation zone of a glacier, as compared to the amount that is melted in the ablation zone.

Tindefjellbreen is a glacier in the municipality of Stryn in Vestland county, Norway. The glacier lies about east of the mountain Skåla, roughly halfway between the villages of Bødalen and Erdalen. The glacier is in the mountains east of the lake Lovatnet and south of the lake Oppstrynsvatn. The glacier is part of Jostedalsbreen National Park, about east of the village of Loen.

Pyne Glacier () is a glacier east of Robson Glacier in the Gonville and Caius Range. It flows north and joins the Mackay Glacier system southwest of The Flatiron. Named after Alex Pyne, recipient of the Polar Medal for services in Antarctic geological and in particular glacial research since 1977; as of January 200 he works at Victoria University's Antarctic Research Centre in Wellington.

Linehan Glacier () is a glacier, long, in Antarctica. It flows northeast from Prince Andrew Plateau along the north side of Turnabout Ridge to enter Lowery Glacier. Linehan Glacier was named by the Advisory Committee on Antarctic Names for Father Daniel Linehan, S.J., who made seismic soundings of ice thickness from , 1954–55, and in the Ross Sea area, 1955–56.

Harbord Glacier () is a glacier in Antarctica, flowing along the south side of Mount George Murray. It enters the Ross Sea south of Whitmer Peninsula where it forms Harbord Glacier Tongue. The name derives from the glacier tongue, which was named by Ernest Shackleton for A.E. Harbord, second officer of the Nimrod during the last year of the British Antarctic Expedition, 1907–09.

View of the glacier over the San Rafael Lake. Non-indigenous people first explored the area of Laguna San Rafael in the year 1675. The glacier of the same name was a land-terminating glacier during that time. It probably reached again the lagoon at some time between 1741 and 1766, and it has been a tidewater glacier since that date.

Kitticarrara Glacier () is a short, steep glacier south of Howard Glacier in the Kukri Hills, flowing east-southeast into Ferrar Glacier, in Victoria Land, Antarctica. It was named by the Western Journey Party, led by Thomas Griffith Taylor, of the British Antarctic Expedition, 1910–13. The name was suggested by Frank Debenham after Kitticarrara, a sheep station in New South Wales.

Colchuck Glacier is in the Stuart Range immediately north of Colchuck Peak and Dragontail Peak, in the U.S. state of Washington. Colchuck Glacier is within the Alpine Lakes Wilderness of Wenatchee National Forest. The glacier is approximately in length, in width at its widest and descends from , where it terminates on barren rock and talus. Below the glacier lies Colchuck Lake.

Sholes Glacier is located on the northeast slopes of Mount Baker in the North Cascades of the U.S. state of Washington. The glacier lies on the north side of the ridge known as The Portals. Between 1850 and 1950, Sholes Glacier retreated . During a cooler and wetter period from 1950 to 1979, the glacier advanced but between 1980 and 2006 retreated back .

Akaga Glacier (, ) is the 5.7 km long and 2.2 km wide glacier on Nordenskjöld Coast in Graham Land situated south of Sinion Glacier and north of the glacier featuring Arrol Icefall. It drains the southeast slopes of Detroit Plateau, flows east-southeastwards and enters Odrin Bay in Weddell Sea. The feature is named after the Bulgar woman ruler Akaga (6th century).

Location of Pernik Peninsula on Loubet Coast, Antarctic Peninsula. Koriten Glacier (, ) is the 5.5 km long and 1.3 km wide glacier on Pernik Peninsula, Loubet Coast in Graham Land, Antarctica, situated northwest of Wilkinson Glacier. It flows southwestwards from Protector Heights and enters the head of Chepra Cove. The glacier is named after the settlement of Koriten in Northeastern Bulgaria.

Il Polo Glacier () is a small glacier draining northward between Polar Times Glacier and Polarforschung Glacier into the Publications Ice Shelf, Antarctica. It was delineated in 1952 by John H. Roscoe from air photos taken by U.S. Navy Operation Highjump, 1946–47, and was named by Roscoe for Il Polo, a polar journal published by the Istituto Geografico, Forlì, Italy.

Astro Glacier () is a glacier in Antarctica, between the Turner Hills and Tricorn Peak in the Miller Range, flowing northeast into the Marsh Glacier. It was seen by the northern party of the New Zealand Geological Survey Antarctic Expedition (1961-62) and so named because an astronomical station was set up on the bluff at the mouth of the glacier in December 1961.

The glacier seen from the southwest (August 2016) The Mittivakkat Glacier is located in southeast Greenland, and is part of the largest ice field on Ammassalik Island. This glacier has been in retreat (negative net mass balance) throughout most of recorded history (1898–2008). Reindeer bones were recovered from the retreating glacier in 2005, and dated to about 1200-1300 AD.

Sandalee Glacier is in North Cascades National Park and Lake Chelan National Recreation Area in the U.S. state of Washington, on the north and east slopes of McGregor Mountain. Sandalee Glacier originates in several cirques and extends from above sea level across a distance of almost . The National Park Service is currently studying Sandalee Glacier as part of their glacier monitoring project.

Boulder Glacier was photographed in 2007 by researchers from the U.S. Geological Survey and those images demonstrate that the glacier has almost disappeared. Earlier images taken in 1910 depict a glacier that was far larger than what was recorded in 2007. Boulder Glacier was far larger when this image was taken in 1910. Compare to the image in the infobox upper right.

Bacon Glacier is a glacier in Juneau City and Borough, Alaska, US, close to the Canada–United States border. It drains into Bacon Creek. The glacier has an elevation of , and is located at . Like many other place names in Alaska, Bacon Glacier also reflects the importance of food to the early prospectors and miners who came up with many of those names.

Garden Glacier is in Wenatchee and Mount Baker-Snoqualmie National Forests in the U.S. state of Washington. Garden Glacier is in two sections, located on the south and east slopes of Sinister Peak. The glacier is along the original approach route for the first ascent of Sinister Peak in 1939. Garden Glacier extends from and end in icefalls and barren rocks.

In the case of positive mass balance, the glacier will continue to advance expanding its low elevation area, resulting in more melting. If this still does not create an equilibrium balance the glacier will continue to advance. If a glacier is near a large body of water, especially an ocean, the glacier may advance until iceberg calving losses bring about equilibrium.

Marble Creek Glacier is in North Cascades National Park in the U.S. state of Washington. Marble Creek Glacier is at the headwaters of Marble Creek, a major tributary of the Cascade River. The glacier lies to the NNW of Dorado Needle and is also NNW of Eldorado Peak. To the east of Marble Creek Glacier lie the much larger Inspiration and McAllister Glaciers.

Dakshini Chamrao glacier, Balbala glacier and Paschimi Kamet glacier all the glacier drain their water in the Saraswati River which then joins Alaknanda River at Keshav Prayag near Mana village. Alaknanda River is one of the main tributaries of river Ganga that later joins Bhagirathi River the other main tributaries of river Ganga at Devprayag and became Ganga there after.

A proglacial river in front of Matanuska Glacier in Alaska, USA. A proglacial river is a river that flows from the margin of a glacier. These rivers are strongly affected by the highly-seasonal water supply from the glacier and by the large supply of sediment that arrives at the glacier terminus. This high sediment supply often makes them steep and braided.

The glacier has its feeding area at 1200 m altitude on the southern flank of the Takhinsha Mountains in the Alsek Ranges.Casement Glacier MapCarta. There it borders the Davidson Glacier, which in contrast flows east to the Lynn Canal. The Casement glacier, with an average width of 1.8 km, flows in predominantly south-southwest direction and ends at about 300 m.

Mount Bonney, is a mountain summit located in Glacier National Park in the Selkirk Mountains of British Columbia, Canada. Mount Bonney is surrounded by ice including the Bonney Glacier, Clarke Glacier, Swanzy Glacier, and Bonney Névé. Its nearest higher peak is Mount Sir Donald, to the northeast. Mount Bonney is visible from Highway 1, the Trans-Canada Highway at Rogers Pass.

White River Glacier is located in the Glacier Peak Wilderness in the U.S. state of Washington. The glacier is within Wenatchee National Forest and nearly touches Honeycomb and Suiattle Glaciers, separated from them by an arête off the Kololo Peaks at its uppermost reaches. White River Glacier has retreated approximately since the end of the Little Ice Age around the year 1850.

Location of Davis Coast on the Antarctic Peninsula. Pirin Glacier (, ) is the 5.7 km long and 6 km wide glacier situated next east of Chavdar Peninsula on Davis Coast on the Antarctic Peninsula. Situated west of Wright Ice Piedmont, north of Gregory Glacier and east of Samodiva Glacier. Draining north- northwestwards from Boulton Peak to enter Curtiss Bay east of Seaplane Point.

The glacier has a relatively high rate of moraine materials, consisting of "friable phyllites and schistose grauwackes". At the foot of the glacier is a lake that was created by glacier recession. Reports from 1892 and 1934 indicated it had "an anomalously slow lake development". The Douglas River (formerly known as the Twain) begins in the lake at the foot of the glacier.

Jeffers Glacier is a glacier located in the Olympic Mountains in Olympic National Park. The body of ice, relatively small compared to the nearby Hoh Glacier, is located southeast of Mount Olympus. Beginning at the foot of a very steep headwall at about , the glacier descends northeast to about before terminating. Meltwater from the terminus flows to the Queets River.

Kintla Glacier is in Glacier National Park in the U.S. state of Montana. The glacier is situated on a plateau southwest of Kintla Peak at an elevation between and above sea level. The glacier has numerous crevasses and is actually two glaciers with a combined area of as of 2005. This is a 34 percent decrease in area from 1966.

Leap Year Glacier () is a tributary glacier between Molar Massif and Mount Stirling in the Bowers Mountains of Antarctica, draining southeast into Black Glacier. It was so named by the northern party of the New Zealand Geological Survey Antarctic Expedition, 1963–64, as party members arrived here in the new leap year of 1964 after climbing out of the Sledgers Glacier.

Chernoochene Glacier (, ) is the 5 km long and 2 km wide glacier on Oscar II Coast, Graham Land in Antarctica situated in the southeast foothills of Forbidden Plateau south of Jorum Glacier and northeast of Crane Glacier. It is draining southeastwards to flow into Spillane Fjord west of Mount Birks. The feature is named after the settlement of Chernoochene in southern Bulgaria.

Blackwall Glacier () is a tributary glacier, long, which drains a portion of the west slope of Nilsen Plateau. It flows northwest along the northeast side of Hansen Spur to join Amundsen Glacier. The name was used by both the 1963–64 and 1970–71 Ohio State University field parties at Nilsen Plateau; all the rock walls surrounding this glacier are black in appearance.

Map of the Mount Conness area The Conness Glacier is on the steep northeast cirque of Mount Conness, east of the Sierra Nevada crest, in the U.S. state of California. The glacier is situated at about . and can be seen from Saddlebag Lake to the east. The glacier is the largest glacier in the Sierra Nevada north of Tioga Pass or Highway 120.

Hinman Glacier lies to the north and northwest of Mount Hinman, in the U.S. state of Washington. Hinman Glacier is within the Alpine Lakes Wilderness of Snoqualmie National Forest. The glacier is approximately in length and descends from , where it terminates on barren rock. The western lobe of Hinman Glacier consists of small patches of ice and has essentially disappeared.

Rennick Glacier is broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier reaches the sea. The seaward part of the glacier was photographed by U.S. Navy (USN) Operation Highjump, 1946–47.

Crescent Glacier () is a small alpine glacier in Antarctica. It is located just east of Howard Glacier in the Kukri Hills, flowing north into Taylor Valley in Victoria Land. The glacier was studied by U.S. geologist Troy L. Pewe in December 1957, and was so named by him because of its crescent shape when viewed from the floor of Taylor Valley.

The Brenva Glacier (, ) is a valley glacier, located on the southern side of the Mont Blanc massif in the Alps. It is the second longest and eighth largest glacier in Italy, and descends down into Val Veny, close to Entrèves, near Courmayeur. Over the centuries it has experienced a number of major rock avalanches which have shaped the glacier and influenced its movement.

People believe that it was real. The elders tell that they brought pieces of ice from the other glacier which they thought to be male and dropped the ice pieces on the Kutia Liungma Glacier. Along with people arranged rituals and prayed the god to save them from the glacier advancing. Within two to three years the glacier retreated about 4-5 kilometers.

Taku Glacier is a tidewater glacier located in Taku Inlet in the U.S. state of Alaska, just southeast of the city of Juneau. Recognized as the deepest and thickest alpine temperate glacier known in the world, the Taku Glacier is measured at thick.H., Robert, and Marge Hermans. Alaska's Natural Wonders: A Guide to the Phenomena. Graphic Arts Center Publishing Company, 2000. 70. Print.

Mitev Glacier (, ) is the 2.9 km long and 2.5 km wide glacier on Brabant Island in the Palmer Archipelago, Antarctica situated east of Laennec Glacier. It drains the north slopes of Avroleva Heights and flows northeastwards to enter Hill Bay west of Petroff Point. The glacier is named after the Bulgarian scientist Ivan Mitev (1924–2006) who discovered the sixth heart tone.

Terminus of the Kaskawulsh Glacier Backpackers can visit the Kaskawulsh along the popular Slims River West Trail, which follows the Slims River south for before ending at the summit of Observation Mountain near the toe of the glacier. Backpackers can also follow the Slims River East Route to reach the toe of the glacier, also known as the glacier terminus.

Emmons Glacier is on the northeast flank of Mount Rainier, in Washington. At , it has the largest surface area of any glacier in the contiguous United States. The glacier was named after the geologist Samuel Franklin Emmons after his involvement in a survey of Mount Rainier in 1870. Starting at an elevation of over , the Emmons glacier flows down eastward.

Packwood Glacier is located in the Goat Rocks region in the U.S. state of Washington. The glacier is adjacent to the Pacific Crest National Scenic Trail and in the Goat Rocks Wilderness of Gifford Pinchot National Forest, northwest of Old Snowy Mountain. McCall Glacier is to the east. Like the town of Packwood, the Packwood Glacier is named in honor of William Packwood.

Company Glacier is in Wenatchee National Forest in the U.S. state of Washington, on the north slopes of Bonanza Peak, the tallest non-volcanic peak in the Cascade Range. Company Glacier descends from with several main chutes converging into the main glacier below the level. Company Glacier was used as the approach route when Bonanza Peak was first climbed in 1937.

Jakobshavn has been a name used for this glacier in scientific literature since 1853 when Danish geologist Hinrich Johannes Rink referred to it as Jakobshavn Isstrøm (Danish for Jakobshavn Ice Stream). It is sometimes referred to in the international scientific literature (by glaciologists) as Jakobshavn Isbræ glacier. Isbræ is Danish for glacier. It is also commonly known by the anglicised version, Jakobshavn Glacier.

Location of Alexander Island in the Antarctic Peninsula region. Yozola Glacier (, ) is the 5 km long and 1.7 km wide glacier in the Sofia University Mountains situated in the northern portion of Alexander Island in Antarctica, and draining north-northwestwards between Mount Braun and Balan Ridge to flow into Palestrina Glacier. The glacier is named after Yozola Lake in the Rila Mountain, Bulgaria.

Mazama Glacier is located on the southeast slopes of Mount Adams a stratovolcano in the U.S. state of Washington. Mazama Glacier is in the Yakama Indian Reservation. The glacier descends from approximately to a terminus near . Mazama Glacier has been in a general state of retreat for over 100 years and lost 46 percent of its surface area between 1904 and 2006.

Wilson Glacier is located on the east slopes of Mount Adams a stratovolcano in the U.S. state of Washington. The glacier is within the Yakama Indian Reservation. The glacier descends from approximately to a terminus near . Wilson Glacier has been in a general state of retreat for over 100 years and lost 14 percent of its surface area between 1904 and 2006.

Romer Lake is famous for its impressive Elephant Foot Glacier, a wide piedmont glacier with a strikingly-shaped wide terminal lobe flowing into the lake from the SE in its central part.GoogleEarthElephant Foot Glacier - Amusing Planet View of the Elephant Foot end moraine at Romer Lake. NASA picture of the southern part of Romer Lake with the Elephant Foot Glacier.

Black Rapids Roadhouse is across the Delta River from the Black Rapids Glacier. For three months in 1937 the Black Rapids Glacier made national news by advancing across the valley at the rate of a mile a month-it was known as the "galloping glacier." The long glacier has since retreated, but the moraine can still be seen from Richardson Highway pullout.

Researchers reported Kilimanjaro's glacier retreat was due to a combination of increased sublimation and decreased snow fall. The Furtwängler Glacier is located near the summit of Kilimanjaro. Between 1976 and 2000, the area of Furtwängler Glacier was cut almost in half, from to . During fieldwork conducted early in 2006, scientists discovered a large hole near the center of the glacier.

The long loop Williwaw Nature Trail is accessible through the Williwaw Campground. The trail provides views of the Middle Glacier. At the turnout for the Begich, Boggs Visitor Center is the Byron Glacier Trail as well as several others. The Portage Glacier can be seen on a short cruise on the M/V Ptarmigan; the glacier is no longer visible from the road.

Crescent Glacier is located on the southeast slopes of Mount Adams in the U.S. state of Washington in Gifford Pinchot National Forest. A small subpeak of Mount Adams, named South Butte, rises nearby. Crescent Glacier is close to the Gotchen Glacier which is located just to the east. Crescent Glacier lies in a small south-facing cirque with a steep headwall.

The Allalin Glacier () is a long glacier (2005) situated in the Pennine Alps near the Allalinhorn in the canton of Valais in Switzerland. In 1973 it had an area of . The glacier is bordered on the west by the Allalinhorn, Rimpfischhorn and Strahlhorn. It is not to be confused with the Fee Glacier which lies on the northern flank of Allalinhorn.

The Turtmann Glacier () is a 5 km long glacier (2005) situated in the Pennine Alps in the canton of Valais in Switzerland. In 1973 it had an area of 5.91 km2. The glacier is located north of Bishorn and Weisshorn. On an altitude of 3256m, at the western border of the glacier, lies the Tracuit Hut (French: Cabane de Tracuit).

Klondike Glacier is in Shoshone National Forest, in the U.S. state of Wyoming on the east of the Continental Divide in the Wind River Range. Klondike Glacier is in the Fitzpatrick Wilderness, and descends from the northeastern slopes of Pedestal Peak. The glacier flows east into a proglacial lake and shares a glacial margin with Grasshopper Glacier to the north.

Topographic map of Smith Island. Armira Glacier (, ) is a long glacier on Smith Island in the South Shetland Islands, Antarctica draining the southeast slopes of Imeon Range southeast of Slaveykov Peak and east of Neofit Peak. It is situated southwest of Dragoman Glacier and northeast of Gramada Glacier, and flows southeastward into Yarebitsa Cove on Osmar Strait. Bulgarian early mapping in 2009.

Harp Glacier () is a tributary glacier flowing south from the glacial col west of Harp Hill into Commonwealth Glacier, Taylor Valley, in Victoria Land, Antarctica. It was named by the Advisory Committee on Antarctic Names in 1997, in association with Harp Hill.

Marr Glacier () is a glacier west of Goldman Glacier, flowing north from the Kukri Hills into Taylor Valley, Victoria Land, Antarctica. It was charted by the British Antarctic Expedition under Robert Falcon Scott, 1910–13, who it appears also applied the name.

Tama Glacier () is a glacier flowing to the sea between Tensoku Rock and Manju Rock on the coast of Queen Maud Land. Mapped from surveys and air photos by Japanese Antarctic Research Expedition (JARE), 1957–62, and named Tama-hyoga (ball glacier).

Granite Glacier is located in the US state of Montana. The glacier is situated in the Beartooth Mountains at an elevation of above sea level and is on the north slope of Granite Peak, the highest summit in Montana. The glacier covers approximately .

Charlesbreen is a glacier in Oscar II Land at Spitsbergen, Svalbard. It is located between Gunnar Knudsenfjella and Vegardfjella, and debouches into St. Jonsfjorden from the south side. The length of the glacier is ten kilometers. The glacier is named after Charles Robertson.

Pūanu Glacier () is a glacier that occupies the upper portion of Papitashvili Valley in the Apocalypse Peaks of Victoria Land. Pūanu is a Māori word, meaning "intense cold", and was applied descriptively to this glacier in 2005 by the New Zealand Geographic Board.

Emmanuel Glacier is a glacier in the Royal Society Range of Victoria Land, descending from Mount Lister northwestward between Table Mountain and Cathedral Rocks to enter Ferrar Glacier. It was named by the British Antarctic Expedition, 1910–13, after Emmanuel College, Cambridge, England.

Glacier Peak in upper right corner Glacier Peak is located on the border of Alberta and British Columbia in the Canadian Rockies. It was named in 1894 by Samuel E.S. Allen in reference to the glacier on the northern side of the mountain.

Disraeli Glacier is a glacier on northern Ellesmere Island, Nunavut, Canada.Disraeli Glacier, Canada It lies in Quttinirpaaq National Park, South- West of the Disraeli Fiord. It is believed to have been named after Benjamin Disraeli, a British politician in the mid 1800s.

The Bärglistock (also spelled Berglistock) (3,656 m) is a mountain of the Bernese Alps, located east of Grindelwald in the Bernese Oberland. The mountain is the tripoint between the valleys of the Upper Grindelwald Glacier, the Unteraar Glacier and the Gauli Glacier.

Longstaffbreen is a glacier in Ny-Friesland at Spitsbergen, Svalbard. It is a branch from the ice areas of Åsgardfonna and Valhallfonna, and the glacier debouches into the lake of Femmilsjøen. The glacier is named after Arctic explorer and mountaineer Tom George Longstaff.

Klawatti Peak () is located in North Cascades National Park in the U.S. state of Washington. Klawatti Peak is a nunatak, a peak surrounded by glaciers. These are Klawatti Glacier to the east, McAllister Glacier to the northwest and Inspiration Glacier to the south.

Holgate Glacier is a glacier located in the U.S. state of Alaska, in Kenai Fjords National Park. It flows outward from the Harding Icefield toward Holgate Arm of Aialik Bay. Tour boats from Seward, Alaska offer tourists the opportunity to view the glacier.

Adolf Hoel Glacier (), also known as Hoel Glacier (Hoels Gletscher), is one of the major glaciers in King Christian X Land, Northeast Greenland. Administratively it lies in the Northeast Greenland National Park zone. The area where the glacier flows is remote and uninhabited.

Foraker Glacier is a glacier in Denali National Park and Preserve in the U.S. state of Alaska. The glacier begins in the Alaska Range on the north side of Mount Foraker, moving northwest for . It is the source of the Foraker River.

Kjerulfbreen (Kjerulf Glacier) is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of about 7.5 kilometers, and is debouching into the Trygghamna bay at the northern side of Isfjorden. The glacier is named after Norwegian geologist Theodor Kjerulf.

During high snow level and/or ski season, Glacier Point road terminates at Badger Pass Ski Resort. Under these conditions, the remainder of Glacier Point Road is used for cross-country skiing access to Glacier Point and other destinations in the high country.

Sulphur Glacier is located in Shoshone National Forest, in the U.S. state of Wyoming on the east of the Sunlight Peak in the Absaroka Range. The glacier sits at an elevation of between . Sulphur Glacier is also within the North Absaroka Wilderness.

Leaving the large expanse of ice, the glacier flows down a small valley, it narrows significantly as it turns northwestward. From there on, the glacier is dirty and ends on steep, uneven terrain at about . The glacier gives rise to the Puyallup River.

Mont Durand Glacier, drawing by Jasmin Nelly Weidmann The Mont Durand Glacier () is a 5.9 km long glacier (2005) situated in the Grand Combin massif, Pennine Alps, in the canton of Valais in Switzerland. In 1973 it had an area of 7.5 km².

Retrieved 2019-04-16 During fieldwork conducted early in 2006, scientists discovered a large hole near the center of the glacier. This hole, extending through the remaining thickness of the glacier to the underlying rock, split the glacier in two by 2007.

Dollfusbreen is a glacier in Wedel Jarlsberg Land at Spitsbergen, Svalbard. The glacier has a length of about 1.5 kilometers, is part of the Recherchebreen glacier complex, and is located between Steinegga and Gaimardtoppen. It is named after Arctic explorer Gustav F. Dollfus.

The Spitsbergen glacier Hambergbreen is named after him. The Bjørnøya mountain of Hambergfjellet is named after him. The Hamberg Glacier of South Georgia and the Hamberg Glacier of NE Greenland are named after him. The mineral hambergite was named after him in 1890.

However, glaciologists speculate that the size of the glacier was at its smallest since the 13th century. In 2008, the glacier front had only receded by since the 2007 measurement. The slower melting is explained by the glacier being completely on dry land.

Hooper Glacier is a glacier in the Palmer Archipelago, Antarctica. It was named after Peter R. Hooper by the UK Antarctic Place-Names Committee.

It was named by the UK Antarctic Place-Names Committee after the minor planet Eros in association with nearby Pluto Glacier and Uranus Glacier.

For a given glacier, the two variables are τD, which varies with h, the depth of the glacier, and τB, the basal shear stress.

Since then North Guardian Glacier resumed retreating and thinning and by 2005 the glacier had returned to its minimum length as recorded in 1946.

In Búrfellsdalur is the Búrfell Glacier, which exhibits what is sometimes referred to as a glacier surge. Farms surrounding Búrfellshyrna include Búrfell and Hæringsstaðir.

Joseph Whidbey, master of the Discovery during the 1791–95 Vancouver expedition, found Icy Strait, at the south end of Glacier Bay, choked with ice in 1794. Glacier Bay itself was almost entirely covered by one large tidewater glacier. In 1879 naturalist John Muir found that the ice had retreated almost all the way up the bay, a distance of around . By 1916 the Grand Pacific Glacier was at the head of Tarr Inlet about 65 miles (105 km) from Glacier Bay's mouth.

The glacier is roughly parallel to the direction of the country's active volcanic zone: north-east to south-west. It is about long and wide, and has a slightly narrower point roughly between the lake Hvítárvatn on the Kjölur mountain road to the east and the Þrístapajökull glacier to the west, near another smaller glacier, Eiríksjökull, which is not quite connected to Langjökull. It is the nearest large glacier to Reykjavík. The area of the glacier includes some mountains, e.g.

Bidalgwar Glacier on the west side of Tharkot and Mrigthuni Glacier, Sukhram Glacier, and Sundardunga Glacier on the eastern side, all the glacier flows from north to south. From the eastern side glaciers comes out Sundardunga river that joins Pindari River near Khati village. Pindari river later joins Alaknanda river at Karnaprayag. Alaknanda River is one of the main tributaries of river Ganga that later joins Bhagirathi River the other main tributaries of river Ganga at Devprayag and became Ganga there after.

Arrow Glacier is located near the summit of Mount Kilimanjaro in Tanzania, on the west slope of the peak and is a small remnant of an icecap which once crowned the summit of Mount Kilimanjaro. The glacier is situated at an elevation of between . Arrow Glacier is adjacent to a climbing route known as the Western Breach/Arrow Glacier Route or more commonly, the Lemosho Route. Arrow Glacier is a recently named glacial remnant that may not even exist as of 2011.

The Klinaklini Glacier is a glacier west of the Klinaklini River and head of Knight Inlet the Coast Land District of British Columbia, Canada (51° 28′ 0″ N, 125° 47′ 0″ W).BCGNIS Query Results: Klinaklini Glacier It flows generally southward from Mt. Silverthrone. The glacier is one of the largest glaciers in western North America. The Hakai Institute has installed a weather station and camera above Klinaklini Glacier that will provide data in near real time to scientists and operational users.

Fairchild Glacier is located in the U.S. state of Washington on Mount Fairchild and Mount Carrie in the Olympic Mountains of Olympic National Park. Beginning at an elevation of about along the Baily Ridge, the glacier descends northeast and is northeast of Carrie Glacier. Like all the glaciers in Olympic National Park, Fairchild Glacier has been in a general retreat for over 100 years. The glacier is named for William R. Fairchild, who was a pilot that assisted scientific researchers in the region.

Central and southern Sentinel Range map. Ramorino Glacier () is the long glacier situated northwest of upper Crosswell Glacier and southeast of Cervellati Glacier on the east slope of Sentinel Range in the Ellsworth Mountains, Antarctica. It flows northeastwards between Epperly Ridge and Shinn Ridge, and enters Crosswell Glacier northwest of Mount Segers. The feature was named by US-ACAN in 2006 after Maria Chiara Ramorino, manager of the Italian team that compiled and promulgated the SCAR Composite Gazetteer of Antarctica, 1998–2006.

In the west the Rhône Glacier covered large parts of the Swiss Plateau and reached as far north as the northern Folded Jura and as far south as Lyon. To the northeast, it transitioned without any sharp demarcation into the Linth Glacier and Reuss - Aare Glacier; only the Napf area remaining ice-free. Further to the northeast, the Reuss-Aare Glacier combined with the Rhine glacier. This extended north beyond the present-day River Danube to the area of the Swabian Jura.

Rettenbach glacier in July 2009 The Rettenbach glacier is a glacier in Europe, located near Sölden in the Ötztal Alps of Tyrol, Austria. During the winter, the glacier is accessible by cable car and from spring time by car, using the Gletscherstraße. In late October, the FIS Alpine Ski World Cup season opens with a giant slalom for both genders on the glacier. The races in October 2016 started at an elevation of and finished at , for a vertical drop of .

Topographic map of Smith Island Bistra Glacier (, ) is long and wide glacier on the northwest side of Imeon Range on Smith Island in the South Shetland Islands, Antarctica. It is situated southwest of Chuprene Glacier and northwest of Dragoman Glacier, drains the west slopes of Mount Foster and the north slopes of Slaveykov Peak, and flows northwestwards of Zavet Saddle to enter Drake Passage south of Garmen Point. The glacier is named after the settlements of Bistra in northeastern Bulgaria.

The Glacier Institute (established in 1983) is a 501(c)(3) non-profit corporation located in Columbia Falls, Montana. According to the U.S. National Park Service, the Glacier Institute provides field-based learning experiences to the public, and serves as an official partner to the Glacier National Park, specializing in field seminars.Glacier National Park - The Glacier Institute (U.S. National Park Service) The Glacier Institute also conducts fund-raising activities for its youth programs, which take place at its Big Creek Outdoor Education Center.

This glacier has advanced since 1947, and has been essentially stable since 1992. Perito Moreno Glacier is one of three glaciers in Patagonia known to have advanced, compared to several hundred others in retreat. The two major glaciers of the Southern Patagonia Icefield to the north of Moreno, Upsala and Viedma Glacier have retreated in 21 years and in 13 years respectively. In the Aconcagua River Basin, glacier retreat has resulted in a 20% loss in glacier area, declining from to .

A century later glacier retreat has opened a multi-armed bay more than 30 miles long. The tidewater glacier has divided into three independent glaciers, Yahtse, Tsaa and Guyot Glacier. Other examples of glaciers currently in the retreat phase are South Sawyer and Sawyer Glaciers in Alaska, retreating 2.1 and 2.3 km respectively from 1961 to 2005. In Patagonia an example of a rapidly retreating glacier is the Jorge Montt Glacier which drains into Baja Jorge Montt in the Pacific Ocean.

Hawkins Glacier Head (21426626109) A glacier head is the top of a glacier. Although glaciers seem motionless to the observer they are in constant motion and the terminus is always either advancing or retreating. The accumulation zone is found at the highest altitude of the glacier, where accumulation of material is greater than ablation. On a glacier, the accumulation zone is the area above the firn line, where snowfall accumulates and exceeds the losses from ablation, (melting, evaporation, and sublimation).

Since the glacier was first observed to be forming and actively flowing in the late 1980s, most scientists working on the mountain have referred to it informally as the "crater glacier". That name has been in wide use with the public (at least those who were aware of the glacier's existence) for the two decades since the glacier formed, and has appeared in several scientific publications too. A single scientific paper, the most complete published study of the glacier to date, referred to it as the "Amphitheater glacier," but that name has not been used otherwise. Despite numerous observations and publications about the growing glacier in the late 1990s and early 2000s, no move was made to give the glacier a permanent and official name until late 2004, after the current eruptive cycle began and the new dome began to split the glacier.

In its strictest sense, the Mer de Glace can be considered as originating at an elevation of , just north of the Aiguille du Tacul, where it is formed by the confluence of the Glacier de Leschaux and the Glacier du Tacul. The former is fed by the Glacier du Talefre, whilst the latter is, in turn, fed by the Glacier des Periardes, the vast Glacier du Géant and the broad icefields of the Vallee Blanche. The Glacier du Tacul supplies much more ice than the Glacier de Leschaux. Mer de Glace, circa 1870 However, if the Mer de Glace is considered in its broadest sense (i.e. from source to tongue), it is a compound valley glacier, gaining ice from snowfields that cover the heights directly north of Mont Blanc at an altitude of around 4,000 metres.

Moraine at Dugdale Glacier, ca November 1899 by Carsten Borchgrevink Termination of Moraine at Dugdale Glacier ca November 1899, by Carsten Borchgrevink The Dugdale Glacier is located just below the centre of this map Dugdale Glacier () is a glacier about long, draining northeast from the Admiralty Mountains into Robertson Bay on the north coast of Victoria Land, Antarctica. The geographical feature flows along the west side of Geikie Ridge before coalescing with Murray Glacier just west of Duke of York Island. It was charted by the British Antarctic Expedition, 1898–1900, under Carsten Borchgrevink, who named it for Frank Dugdale of Snitterfield, Stratford-on- Avon. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

Mount Bazarduzu northeast slope glaciers (41°13′28″), Greater Caucasus, Russia/Azerbaijan 2\. Snezhnika glacieret (41°46′09″), Pirin massif, Bulgaria 3\. Banski Suhodol Glacier (41°46′54″), Pirin mountain, Bulgaria 4\. Mertur cirque glacier (42°23’55”), Hekurave range, Prokletije mountains, Albania 5\. Maja Jezercë glaciers and glacierets (42°26’27”), Prokletije mountains, Albania 6\. Calderone glacier (42°28′10”) Gran Sasso massif, Apennine Mountains, Italy 7\. Kolata glacieret (42°29′00”), Kolata massif, Prokletije, Albania/Montenegro 8\. Aneto glacier (42°37′32”), Aneto-Maladeta, Pyrenees, Spain 9\. Posets glacier (42°39′10”), Pyrenees, Spain 10\. Monte Perdido glacier (42°40′38”), Pyrenees, Spain 11\. Mount Dzhimara Glacier (42°43′15″), the european northwestern slopes of Mount Dzhimara, Khokh Range, Greater Caucasus, Russia 12\.

Glitrefonna Glacier () is a glacier at the north side of Mount Bergersen in the Sør Rondane Mountains of Antarctica. It was mapped by Norwegian cartographers in 1957 from air photos taken by U.S. Navy Operation Highjump, 1946–47, and named Glitrefonna (the glitter glacier).

Godwit Glacier () is a glacier that flows northeast from Mount Holm-Hansen into Bartley Glacier in the Asgard Range of Victoria Land, Antarctica. It was named by the New Zealand Geographic Board (1998) after the godwit, a migratory bird which summers in New Zealand.

Français Glacier Tongue () is a broad glacier tongue about long extending seaward from Français Glacier. It was charted in 1951 by the French Antarctic Expedition and named by them for the Français, expedition ship of the French Antarctic Expedition, 1903–05, under Jean-Baptiste Charcot.

Hewson Glacier () is a glacier in the Queen Alexandra Range, Antarctica, long, flowing northeast to enter Beardmore Glacier just north of The Cloudmaker. It was named by the New Zealand Geological Survey Antarctic Expedition (1961–62) for Ronald Hewson, a surveyor with the expedition.

Hull Glacier Hull Glacier () is a glacier, about long, flowing northwest between Mount Giles and Mount Gray into Hull Bay, in Marie Byrd Land, Antarctica. It was discovered by the United States Antarctic Service (1939–41) and named for U.S. Secretary of State Cordell Hull.

McDonald Glacier is in the U.S. state of Montana. The glacier is situated in the Mission Mountains at an elevation of above sea level and is immediately north of McDonald Peak. The glacier covers approximately and is located in a cirque below McDonald Peak.

Ichime Glacier () is a glacier flowing to the sea just west of Kasumi Rock in Queen Maud Land, Antarctica. It was mapped from surveys and air photos by members of the Japanese Antarctic Research Expedition, 1957–1962, who also gave the glacier its name.

Rush Lake and Rush Peak is reached via Nagar and Hopar Valley via the Hopar Glacier (Bualtar Glacier) and Miar Glacier, which rises from Miar and Phuparash peaks. The trek to Rush Lake provides views of Spantik, Malubiting, Miar Peak, Phuparash Peak and Ultar Sar.

Freemanbreen is a glacier on Barentsøya, Svalbard. It is an offshoot of Barentsjøkulen, reaching down to the sea in the southern direction, into Freemansundet. The glacier is named after British Alderman Ralph Freeman. The mountain of Buklerimen separates Freemanbreen from the glacier of Hübnerbreen.

Pinnacle Glacier is in Mount Rainier National Park in the U.S. state of Washington, on the northeast slopes of Pinnacle Peak. Pinnacle Glacier is south of Mount Rainier and is a small remnant glacier that has developed a proglacial lake as it has retreated.

Astudillo Glacier () is a small glacier flowing into Paradise Harbor between Leith Cove and Skontorp Cove on the Danco Coast of Graham Land. The glacier was surveyed by the Chilean Antarctic Expedition of 1950-51, which applied the name, probably after an expedition member.

Lake Frances is located in Glacier National Park, in the U. S. state of Montana. Runoff from the Dixon Glacier empties into the south side of the lake while runoff from Thunderbird Glacier flows into Thunderbird Creek and into the east shore of the lake.

The creek cascades down towards Mendenhall Lake, forming a hanging valley, then plunges over the falls to the lake. Prior to the recession of Mendenhall Glacier, it was said that the falls would drop "directly on the glacier", or that the "glacier covered the waterfall".

Beaglehole Glacier () is a glacier between Spur Point and Friederichsen Glacier on the east coast of Graham Land. It was named by the UK Antarctic Place-Names Committee after John Cawte Beaglehole, New Zealand historian of the Antarctic and biographer of Captain James Cook.

Lillian Glacier was located in the Olympic Mountains in Olympic National Park in the U.S. state of Washington. The remnants of the glacier are in a cirque below McCartney Peak. Between 1905 and 2010, the Lillian Glacier melted away most likely because of global warming.

Rennell Glacier () is a glacier, long, in the Pioneer Heights, Heritage Range. It drains northwest, to the east of Inferno Ridge, to join Splettstoesser Glacier. Named by the University of Minnesota Geological Party to these mountains, 1963–64, for K.P. Rennell, biologist with the party.

In 1959 the Lawrie Glacier Lawrie Glacier on USGS/GNIS on the west coast of Graham Land in Antarctica was officially named. The glacier was first mapped by the British Graham Land Expedition (1934–37) to which Robert Lawrie had supplied boots and equipment.

Vintervegen (Winter Road) is a glacier in Oscar II Land at Spitsbergen, Svalbard. It has a length of about . The glacier borders to the mountain of Klampen, merges with Osbornebreen and other glaciers, and the merged glacier stream debouches into the head of St. Jonsfjorden.

Fleischmann Glacier is a glacier in the Alaska Range of Denali National Park and Preserve in the U.S. state of Alaska. The glacier lies in the southern Kichatna Mountains above Simpson Pass, moving south. It the source of Morris Creek, which feeds the Kichatna River.

Nathorst glacier, Svalbard, in midnight sun Nathorstbreen is a glacier located on the southern part of Spitsbergen, emptying into Van Keulenfjorden. Nathorstbreen is a glacier on Spitsbergen, Svalbard. It has a length of about , and debouches into Van Keulenfjorden. It has several side glaciers.

Scott Glacier is a 15-mile-long (24 km) glacier located in the Chugach Mountains, near Cordova, Alaska. It begins at and trends southwest to , 13 miles (21 km) east northeast of Cordova. The Scott Glacier was named in 1908 after a "local miner".

Topographic map of Livingston Island and Smith Island Argentina Glacier is a glacier flowing northwest from Hurd Dome and terminating near Argentina Cove, South Bay, Livingston Island. The name Argentina Glacier was given in association with Argentina Cove by the Spanish Antarctic Expedition, about 1995.

Argo Glacier () is a glacier in the Miller Range, long, flowing northeast to enter Marsh Glacier just south of Macdonald Bluffs. It was named by the New Zealand Geological Survey Antarctic Expedition (1961–62) after the Argo, the vessel sailed by Jason in Greek mythology.

Abano Glacier is located on the southeastern slope of Mt. Kazbek in the Kazbegi District of Georgia. The length of the glacier is and its surface area is . The maximum width of the Abano Glacier is . Its meltwater is drained towards the river Terek.

Overlooking Chuprene Glacier to the northwest, Pashuk Glacier to the east and Rupite Glacier to the southeast. Bulgarian mapping in 2009 and 2010. Named after the Bulgarian financier, industrialist and philanthropist Evlogi Georgiev (1819–1897) whose endowment funded the construction of Sofia University’s main building.

Saun glacier is situated north to Neola glacier. The snout of the Neola glacier is a one-hour trek along Duktu Nala from Duktu village. The snout of Neola is situated at an altitude of . This place also serves as base camp for Panchchuli expeditions.

Mount Gilmour () is a mountain 4 nautical miles (7 km) southeast of Mount Passel on the central part of the irregular ridge separating Crevasse Valley Glacier and Arthur Davis Glacier (ex-Warpasgiljo Glacier), in the Edsel Ford Ranges of Marie Byrd Land, Antarctica.Mount Gilmour. MapPlanet.

The glacier finishes at its merger with another glacier, the Kronebreen, another surge glacier moving at around 750 metres per year, along a ice front with dirty 5- to 20-metre-high ice cliffs, as the Kongsbreen picks up medial moraine and englacial debris.

The longest glacier is the Kahiltna Glacier. Wintertime activities include dog sledding, cross-country skiing, and snowmobiling. The park received 594,660 recreational visitors in 2018.

Providing overland access from Boyana Glacier to upper Macy Glacier. Bulgarian topographic survey Tangra 2004/05. Named after the settlement of Starosel in central Bulgaria.

The largest and longest glacier in the Alps, the Aletsch Glacier is 23 km long and has a maximum thickness of 900 metres at Konkordiaplatz.

The Chenega Glacier finds its source in the Sargent Icefield. The glacier is the namesake of the Alaska Marine Highway fast ferry M/V Chenega.

The Kaskawulsh Glacier is a vast, temperate valley glacier nestled in the St. Elias Mountains, within Kluane National Park in the Canadian territory of Yukon.

The Leverett Glacier in Antarctica, Leverett Glacier in Greenland, Lake Leverett in Washington (since drained), and plant species Sigillaria leveretti were named after Frank Leverett.

Parke Peak () is located in the Livingston Range, Glacier National Park in the U.S. state of Montana. Harris Glacier is immediately northeast of Parke Peak.

A cable car connects the station at Montenvers with the glacier which is tunnelled out at that point enabling tourists to walk inside the glacier.

Fox Glacier () is a village on the West Coast of the South Island of New Zealand. The village is close to the eponymous Fox Glacier.

Descent Glacier () is a short, steep glacier between Briggs Hill and Condit Glacier, flowing northwest from Descent Pass into Ferrar Glacier, in Victoria Land. It was so named because of the adventurous descent made here by the party led by Albert Armitage of the British National Antarctic Expedition, 1901–04. The name seems to have been first used on maps of the British Antarctic Expedition, 1910–13.

Dilemma Glacier is a steep, broken glacier descending from the Worcester Range into the western side of Skelton Glacier to the north of Ant Hill, in New Zealand. It was mapped and named in 1957 by the New Zealand party of the Commonwealth Trans-Antarctic Expedition, 1956–58, and so named because of difficulties encountered by the geological party in an attempted descent of this glacier.

The Tordrillos are primarily a volcanic range, like most of the neighboring Aleutian Range; however some of the peaks (for example, Mount Torbert) are not volcanoes. Mount Spurr, the southernmost peak in the range, had its most recent eruption in June 1992. They are heavily glaciated, partly due to their location near Cook Inlet. Major glaciers include the Capps Glacier, Triumvirate Glacier, Hayes Glacier, and Trimble Glacier.

Pipecleaner Glacier () is a glacier formed by the coalescence of numerous small alpine glaciers on the east side of Mount Huggins. Together with Glimpse Glacier it joins the Radian Glacier where that stream meets the north arm of Dismal Ridge. Its surface is marked by innumerable bands of moraine reminiscent of pipecleaners. Named by New Zealand Victoria University of Wellington Antarctic Expedition (VUWAE), 1960–61.

Pitkevitch Glacier () is a glacier, 20 nautical miles (37 km) long, flowing north from the Admiralty Mountains along the west side of DuBridge Range. The glacier reaches the sea just east of Atkinson Cliffs, where it forms Anderson Icefalls. A portion of the terminus merges northwestward with Fendley Glacier. Mapped by United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1960–63.

Gray Glacier () is a glacier in the Cobham Range, Antarctica. It is long, lies south of Tarakanov Ridge and flows southeast to merge with Prince Philip Glacier where the two join Nimrod Glacier. It was named by the Holyoake, Cobham, and Queen Elizabeth Ranges party of the New Zealand Geological Survey Antarctic Expedition (1964–65) for M. Gray, postmaster and assistant radio officer at Scott Base, 1965.

Mollweide Glacier () is a steep glacier south of Mount Kowalczyk, descending west from Hobbs Ridge into Blue Glacier, in Victoria Land, Antarctica. The name is one of a group in the area associated with surveying applied in 1993 by the New Zealand Geographic Board; this glacier was named from the Mollweide projection, an equal area map projection with the parallels and central meridian being straight lines.

Lowe Glacier () is a tributary glacier long in the Queen Elizabeth Range, Antarctica. It flows south from a common saddle with the Prince of Wales Glacier east of Mount Gregory to join the Princess Anne Glacier. The name was proposed by the Holyoake, Cobham and Queen Elizabeth Ranges Party of the New Zealand Geological Survey Antarctic Expedition, 1964–65, after D. Lowe, a member of the party.

The Hooker River is a river in the Southern Alps of New Zealand. It flows south from Hooker Lake, the glacier lake of Hooker Glacier, which lies on the southern slopes of Aoraki / Mount Cook. After 3 kilometers, it flows through Mueller Glacier Lake, gathering more glacial water, before joining the braided streams of the Tasman River, also an outflow of a glacier lake.

There are several locations within the park from which the glacier can be viewed. The only vista available from the road, however, is from the Wheeler Peak Overlook on the Wheeler Peak Scenic Drive. The glacier can be seen at the bottom of the Wheeler Peak rock face. The Bristlecone/Glacier Trail can be used to access the foot of the glacier, and is approximately roundtrip.

Evison Glacier () is a small glacier draining from the south end of Molar Massif in the Bowers Mountains of Victoria Land, Antarctica. This glacier was so named by the New Zealand Geological Survey Antarctic Expedition, 1967–68, for F.F. Evison, New Zealand's first professor of geophysics. The glacier lies situated on the Pennell Coast, a portion of Antarctica lying between Cape Williams and Cape Adare.

View of the Blackcomb Glacier from the top of Horstman Glacier The Horstman Glacier is a glacier located on Blackcomb Peak in Garibaldi Provincial Park. During the ski season at Whistler Blackcomb Ski Resort, it is used for skiing and riding on. During the summer ski season on Blackcomb Peak, it is one of two glaciers in the North America used for summer skiing and riding.

Man-o-War Glacier () is a tributary glacier in the Admiralty Mountains of Antarctica. It drains the vicinity south of Mount Black Prince and Mount Royalist and flows southward to enter Tucker Glacier between the McGregor Range and Novasio Ridge. The glacier was named for a "man-o-war" in association with the Admiralty Mountains by the New Zealand Geological Survey Antarctic Expedition of 1957–58.

Upper Grinnell Lake is located in Glacier National Park, in the U. S. state of Montana. Upper Grinnell Lake is a proglacial lake which formed in the 1930s as Grinnell Glacier retreated. The lake is often filled with small icebergs which have been breaking off Grinnell Glacier. Upper Grinnell Lake can be reached by trail and is a hike from the Many Glacier Hotel.

Seafarer Glacier () is a tributary glacier draining southward from Webb Névé, between the Lawrence Peaks and Malta Plateau, to enter Mariner Glacier, in Victoria Land. So named by the Mariner Glacier party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1966–67, both in association with the name Mariner, and also with the `Seafarer', the Anglo-Saxon fragment-poem about travel over icy seas.

Avalanche Glacier is located on the west to southwest slopes of Mount Adams a stratovolcano in the Gifford Pinchot National Forest in the U.S. state of Washington. The glacier descends from the White Salmon Glacier at to a terminus near . Avalanche Glacier has been in a general state of retreat for over 100 years and lost 59 percent of its surface area between 1904 and 2006.

Aleksiev Glacier (, ) is the 10.5 km long and 3 km wide glacier on Nordenskjöld Coast in Graham Land situated northeast of Kladorub Glacier and south of the glacier featuring Arrol Icefall. It drains the southeast slopes of Detroit Plateau, and flows east-southeastwards to enter Desislava Cove in Weddell Sea. The feature is named after the Bulgarian artist and writer Rayko Aleksiev (1893–1944).

Sentinel Range map. Divdyadovo Glacier (, ) is the long and wide glacier in Petvar Heights on the southeast side of Sentinel Range in Ellsworth Mountains, Antarctica situated northeast of Carey Glacier and southeast of Drama Glacier. It is flowing northeastwards, then north of Ruset Peak turning east- southeastwards to leave the range southeast of Long Peak. The feature is named after the settlement of Divdyadovo in northeastern Bulgaria.