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146 Sentences With "snow free"

How to use snow free in a sentence? Find typical usage patterns (collocations)/phrases/context for "snow free" and check conjugation/comparative form for "snow free". Mastering all the usages of "snow free" from sentence examples published by news publications.

An estimated 479,000 people usually visit during the snow-free period.
That might be fine (if occasionally treacherous) in snow-free cities.
By combining several mats, an entire sidewalk area can be kept ice and snow-free.
On a snow-free weekend, when normally the lake would be dead, streets were swarming with families.
The skier is in the perfect inverted position, mid-air between the snow-free hills in the background.
It's largely snow-free right now, Mr. Hamrick said, but it's windy in eastern Montana and South Dakota.
On March 18th, they are all mostly snow-free with the exception of Western New York and the Appalachians.
No, it's not a protective garment you wear to keep your neck snow-free (although that could also come in handy!).
Early last week, the valleys of Vermont were largely snow-free, and a majority of its mountain peaks were still dry and green.
As he strode across a snow-free White House South Lawn toward his helicopter, Obama joked he'd cleared the wide swath of grass himself.
Much further down the mountain, I treated myself to a short, snow-free, moss-filled hike to see Mill Creek Falls off Highway 113.
Any other winter, the lanes would have been laden with natural drifts, said 153-year-old jogger Marie Sten, back from a run along the forest's snow-free paths.
MOSCOW (Reuters) - Inured to interminable winters, Muscovites have been stunned this year by spring-like temperatures and virtually snow-free sidewalks after the Russian capital recorded its warmest January in history.
Luckily it held off long enough for the game to go on as people helped clear off the parking lots and field, and St. Mirren's field has a heating system that helped keep it snow-free.
His mother hails from County Galway on Ireland's rugged, and mostly snow-free, west coast, and though her son was born in a land where cross-country skiing is a national obsession, he said he always wanted to wear the green.
But previous visits to Lapland had forewarned me that a pan-flat eternity of snow-free wood and melted water might not make for a gripping first or last chapter, so I pedaled my shopping bike out of Kirkenes — the trail's top-end start point — in a mid-March blizzard.
It is snow free in the summer time, a simple walk up.
Scale 1:120000 topographic map. Troyan: Manfred Wörner Foundation, 2010. (First edition 2009. ) — is snow-free in summer.
Scale 1:120000 topographic map. Troyan: Manfred Wörner Foundation, 2009. (Updated second edition 2010. ) and is snow-free in summer.
For example, snowfields commonly accumulate on the lee sides of ridges while ridgelines may remain nearly snow free due to redistribution by wind. Some alpine habitats may be up to 70% snow free in winter. High winds are common in alpine ecosystems, and can cause significant soil erosion and be physically and physiologically detrimental to plants. Also, wind coupled with high solar radiation can promote extremely high rates of evaporation and transpiration.
Whilst limitations of space dictated that the triangle had to be partly constructed in tunnels it also ensures that in winter it is snow- free and is readily available in emergencies.
For both directions plan around 5 hours to get to the summit. The route from the south starts in the Fionnay valley (Val de Bagnes) and it is snow-free in summer time.
Grass flourishes in warmer Antarctic originally from The Times, December 2004 Climate change is leading to a mismatch between the snow camouflage of arctic animals such as snowshoe hares with the increasingly snow-free landscape.
Both approaches involve a strenuous 16-mile+ round trip with over 4000 feet of climbing. The hike often takes all day. The hike is most accessible in the snow-free months of summer and fall.
Mean annual precipitation is 30.4 inches with 75% occurring in the snow-free period. The pH of waters in the bogs range from about 3.5 to 4.5 with the fens having a pH of near neutral.
Since Tukudika were aware migratory patterns of deer and elk and bighorn sheep, they likely migrated out of high elevations to spend winter at the mouth of mountain canyons where they spill out to the plains, or in the basins themselves. Some big game wintering areas, such as Sunlight Basin and the upper Wind River Valley, are nearly snow-free in winter. Other recent excavations have suggested that certain snow-free areas within the Wind River Range may have been used by Indians in mid-winter for up to 12,000 years.
The Goorkha Craters () are a line of snow-free coastal hills long, standing east of Cooper Nunatak between Carlyon Glacier and Darwin Glacier in Antarctica. They were discovered and named by the British National Antarctic Expedition ( (1901–04).
Most years the wilderness is still buried under of snow in May. Usually most trails and passes are snow free by mid-August, but this varies from year to year. Snow and cold rain can occur in mid-summer.
Topographic map of the Cape Hallett area Cape Hallett is a snow-free area (Antarctic oasis) on the northern tip of the Hallett Peninsula on the Ross Sea coast of Victoria Land, East Antarctica. Cape Adare lies to the north.
Victoria is popular with boaters with its rugged shorelines and beaches. Victoria is also popular with retirees, who come to enjoy the temperate and usually snow-free climate of the area as well as the usually relaxed pace of the city.
Syrtis Hill () is a prominent snow-free conical terraced hill, rising to about 500 m, on the northwest corner of the Two Step Cliffs massif overlooking Viking Valley, in the southeast portion of Alexander Island, Antarctica. The hill is an important snow-free landmark and the site of biological and geological research. Named by United Kingdom Antarctic Place-Names Committee in 1993 after Syrtis Major Planum, the prominent dark feature on the planet Mars, first described by the Dutch astronomer Huygens in 1659. This hill was most likely named in association with nearby Mars Glacier and Planet Heights.
The climatic snow line is the boundary between a snow-covered and snow-free surface. The actual snow line may adjust seasonally, and be either significantly higher in elevation, or lower. The permanent snow line is the level above which snow will lie all year.
They also have the advantage of being snow- free for longer than the adjoining subranges of the Allgäu Alps to the south. The mountains consist of four rock groups. In the northernmost ridges molasse is dominant. In places flysch is represented, as is main dolomite.
It has a very local distribution, confined to open ground and mountain summit plateaux that are sufficiently exposed to be kept snow-free. Its native distribution includes Iceland, Svalbard, northern Norway and Scottish mountains and mountains of Western North America and the Kamchatka peninsula.
Bareface Bluff () is a large, sheer snow-free bluff, high, rising above Skelton Glacier, between Ant Hill Glacier and Mason Glacier in Antarctica. It was surveyed and given this descriptive name in 1957 by the New Zealand party of the Commonwealth Trans-Antarctic Expedition, 1956-58\.
Mount Barsoum () is a pointed and partly snow-free peak on the west end of Martin Hills. It was positioned by the U.S. Ellsworth-Byrd Traverse Party on December 10, 1958 and was named for Lieutenant Adib H. Barsoum, U.S. Navy, Medical Officer at Ellsworth Station in 1958.
Most parts of Waldershof belong to the nature park Steinwald. The climate is unique to this region and has Alpine characteristics. Area's near or in the forest are sometimes not snow-free until the middle of May. Giant snowdrifts and severe snow storms render paths and trails impassable in winter.
Vegetation is particularly common on a ridge within and south of the main crater, "Cryptogam Ridge". It features a long snow-free area with a gravelly ground, small terraces and stone stripes. Soil temperatures recorded there reach . These are the only occurrences of Campylopus pyriformis on warm ground in Antarctica.
Mount McCoy () is a high table-topped massif with dark, snow-free, vertical walls, at the east side of Land Glacier in Marie Byrd Land, Antarctica. It was discovered by members of West Base of the United States Antarctic Service (1939–41) and named for James C. McCoy, chief pilot at West Base.
Later chapters set in snow-free forest were largely filmed in the Big Bear Lake region of California's San Bernardino National Forest."Canadian Mounties vs. Atomic Invaders: Files of Jerry Blake" (undated), , Retrieved January 13, 2014 It was filmed between 24 March and 13 April 1953. The serial's production number was 1936.
February was a mild month (the 9th mildest in the last century) with very little frost and much of the country having its first snow-free February since 1998. The only significant wintry weather came on the 18th-21st when some overnight dustings of snow fell as far south as the Midlands.
The climate in the Steinwald has Alpine characteristics. It is not snow-free until the middle of May. Giant snowdrifts and severe snow storms render paths and trails impassable in winter. A short spring follows the long and harsh winter; summer has more precipitation and is followed by a mild and fine autumn.
Probe Ridge () is a prominent, snow-free, terraced ridge forming part of the north flank of Viking Valley, situated in the southeast portion of Alexander Island, Antarctica. The ridge was named by the United Kingdom Antarctic Place- Names Committee (UK-APC) in 1993 after the space probe which surveyed the planet Mars in 1976.
Mariner Hill () is a prominent snow-free conical hill, rising to about midway between Syrtis Hill and Two Step Cliffs, situated in the southeastern portion of Alexander Island, Antarctica. It was named by the UK Antarctic Place-Names Committee in 1993 after Mariner 9, the NASA probe which was the first spacecraft to orbit the planet Mars, in 1971.
Mount Sabine is a prominent, relatively snow-free mountain rising between the heads of Murray Glacier and Burnette Glacier. Discovered on January 11, 1841, by Captain James Ross, Royal Navy, who named this feature for Lieutenant Colonel Edward Sabine of the Royal Artillery, Foreign Secretary of the Royal Society, one of the most active supporters of the expedition.
The Racherin, a mountain with a height of , lies in the Glockner Group in the High Tauern range in Austria. The summit is located ca. 6 km, as the crow flies, northwest of Heiligenblut in the state of Carinthia. The unmarked and mostly trackless normal route is not difficult in snow-free and dry conditions, but is rather laborious.
Spring and fall are pleasantly mild but prone to drastic temperature changes; spring even more so than fall. Late season heat waves as well as "Indian summers" are possible. Early and late season snow storms can occur in November and March, and more rarely in April. Montreal is generally snow free from late April to late October.
The region of the Nordenskjöld Coast has particularly steep slopes on the coast, with high covered ice plateaus. Cape Sobral lies 12 miles from Cape longing. It is a high plank of rock that is projected above the water below, and is partly snow free. Behind Cape Sobral is a deep fiord that is surrounded by glaciers, which extends to Palmier Peninsula.
Mount Harvey () is a snow-free peak east of Amundsen Bay, standing in the Tula Mountains of Antarctica, about east-northeast of Mount Gleadell. It was sighted in 1955 by an Australian National Antarctic Research Expeditions party led by P.W. Crohn, and was named by the Antarctic Names Committee of Australia for William Harvey, a carpenter at Mawson Station in 1954.
During the short summers, much of Northern Canada is snow free, except for the Arctic Cordillera which remains covered with snow and ice throughout the year. In the summer months, temperatures average below and may occasionally exceed . Most of the rainfall accumulated occurs in the summer months, ranging from in the northernmost islands to at the southern end of Baffin Island.
Beaudoin Peak () is a snow-free peak, high, surmounting the southeast part of the Meyer Hills in the Heritage Range. It was mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1961–66, and named by the Advisory Committee on Antarctic Names for Douglas W. Beaudoin, United States Antarctic Research Program meteorologist at Ellsworth Station, 1961.
Location of Snow Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Pazardzhik Point (, ‘Nos Pazardzhik’ \'nos 'pa-zar-dzhik\\) is a point on the southeast coast of Snow Island in the South Shetland Islands, Antarctica situated 2.1 km east- northeast of Cape Conway and 9.9 km southwest of Hall Peninsula. Snow-free in summer.
Holme Bay is a bay in Antarctica in Mac. Robertson Land, wide, containing many islands, indenting the coast north of the Framnes Mountains. Holme Bay is largely snow-free and was mapped by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition in January-February 1937, and named Holmevika because of its island-studded character (holme means "islet" in Norwegian) .
In northern Alaska, the melt-date has advanced by 8 days since the mid-1960s. Decreased snowfall in winter followed by warmer spring conditions seems to be the cause for the advance. In Europe, the 2012 heat wave has especially been anomalous at higher altitudes. For the first time on record, some of the highest Alpine peaks in Europe were snow- free.
Milliken, a residential Scarborough neighbourhood, during an ice storm, on 15 April 2018. Despite being cold, extended snow free periods occur in most winter seasons and precipitation can fall as rain with temperatures sometimes climbing above . Average winter snowfall is at the weather station in Downtown Toronto and at Toronto Pearson International Airport. The average January maximum/minimum is / in the city.
After crossing the three valleys of Lanzo Torinese, the Susa Valley is reached after 26 sections. This is the approximate midpoint of the GTA, and the boundary between its northern and southern parts. In the Cottian Alps, between the Susa and Varaita valleys, were several variants of the GTA. An eastern route, snow-free by early June, is neglected; the main, western route is well-maintained.
North Suicide Peak is accessible via the popular Falls Creek, McHugh Creek, and Rabbit Lake trails. In the summer months, it is a rugged but non-technical climb that is typically completed as a day trip from nearby Anchorage, Alaska. The peak can be climbed in all seasons but is most popular in the summer and fall, when the majority of the mountain is snow-free.
To the north of Patriot Hills (in their slipstream) there is an approximately 2x8 km large blue ice rink, a snow-free surface that can be used as a landing strip for large aircraft including C130 and Ilyushin Il-76 .National Science Foundation: INITIAL ENVIRONMENTAL EVALUATION DEVELOPMENT OF BLUE-ICE AND COMPACTED-SNOW RUNWAYS IN SUPPORT OF THE U.S. ANTARCTIC PROGRAM. 9. April 1993.
The Meadows-in-the-Sky Parkway is a paved mountain road open during the snow free months. The parkway begins in the rainforests of the park's southwest corner, winds upward through the sub- alpine forests and ends in the rolling sub-alpine wildflower meadows. The Monashee Mountains rise to the west, with the Selkirk range to the east. Giant Cedars Boardwalk is a 500 m.
The average annual sunshine hours are 2797.1 hours, and the annual average temperature is 6.5 °C. The average annual frost-free period is 171 days and average annual snow-free days are 99 days. The average annual precipitation is 199.1 mm and annual precipitation days are 65– 80 days. The average annual evaporation is 1535.1 mm and an average annual wind speed of 1.7 m/s.
By 2010 the two herds, separated by glaciers terminating in the ocean and isolated from other ice and snow free areas, comprised some 2600 animals occupying 318 km2, one third of the total vegetated area, and thus potential grazing habitat, of the island.Christie (2010). An accurate count during the eradication of 2013-15 showed that earlier estimates of numbers were very low - nearly 7,000 were killed.
Huts serving the peak are the Cabane de Tracuit (3,256 m) and the Turtmann hut (2,519 m). Access to both huts is snow- free in summertime. The Tracuit hut is normally accessed from the Zinal valley, a long and demanding walk of around five hours from the village to the hut. The Turtmann hut is primarily used for climbing the Barrhorn and the Brunegghorn.
Haven Mountain is a prominent mountain, high, with a level razor-back snow ridge at its highest (eastern) part, standing northeast of the Three Nunataks in the northwestern part of the Britannia Range. It was so named by the Darwin Glacier Party of the Commonwealth Trans-Antarctic Expedition (1956–58), who sheltered for five days in the largely snow-free area below the north side of the summit ridge.
There seems to be a variety of qualifiers for appropriate nest sites. The nest site is typically snow-free and dry relative to the surrounding environment, usually with a good view of the surrounding landscape. The nest may be made of ridges, elevated mounds, high polygons, hummocks, hills, man-made mounds and occasionally rocky outcrops. If covered with vegetation, taller plants that may obstruct view are plucked away sometimes.
The GTA then enters the Ligurian Alps, ending at Viozene in Ormea. Trail extensions continue to the train stations at Ormea or Gerassio, cross to the Alta Via dei Monti Liguri or lead to the Mediterranean Sea (which can be reached in about three days from Ormea). The GTA is usually snow-free at the end of June. A mountain trail, it has no technical difficulties; however, trail marking is irregular.
The peninsula is the most extensively snow-free coastal area in summer on the island, most of which is permanently covered by ice. Its southeastern end is a point called Halfthree Point. It was charted and named by Discovery Investigations personnel on the Discovery II in 1935. It is part of the Fildes Peninsula Antarctic Specially Protected Area (ASPA 125), designated as such because of its paleontological values.
The species is heat-sensitive but prefers snow-free, grass-dominated areas near escape cliffs, and in terrain that is difficult for humans and livestock to reach. A fragment of a land with optimal terrain, climate, and degree of human disturbance for the species' occurrence is more likely to contain the species if the area of the fragment is larger and its distance to the species' nearest source population is shorter.
Siberian cranes return to the Arctic tundra around the end of April and beginning of May. The nest is usually on the edge of lake in boggy ground and is usually surrounded by water. Most eggs are laid in the first week of June when the tundra is snow free. The usual clutch is two eggs, which are incubated by the female after the second egg is laid.
Location of Snow Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Mikre Beach (, ) is the beach extending 2.2 km on the southeast coast of Snow Island in the South Shetland Islands, Antarctica. It is bounded by Cape Conway to the southwest, the island's ice cap to the northwest and Pazardzhik Point to the northeast, and is snow-free in summer.
The scarcity and poor quality of road infrastructure limits land transportation by conventional vehicles. A normal car on tires has very limited capability for Antarctic conditions. Scientific bases are often built on snow free areas (oases) close to the ocean. Around these stations and on a hard packed snow or ice, tire based vehicles can drive but on deeper and softer snow, a normal tire based vehicle cannot travel.
Fog too is more common in the summer, occurring on roughly one-third of the days. The island receives about of precipitation per year, with the highest monthly totals occurring between late summer and early winter, when Bering Sea storms batter the island. Snowfall levels are highest between December and March, averaging per year. Other than trace amounts, the period from June to September is generally snow-free.
There are few reports of ribbed bog moss's elevational tolerances. Ribbed bog moss is reported from 1,600 to 5,700 feet (500-1,750 m) in west-central Alberta and at 827 feet (252 m) in Kosciucko County, Indiana. In subalpine and alpine communities of the North Cascade Range in Washington and British Columbia, ribbed bog moss occurs on high-elevation (>7,380 feet (2,250 m)) sites that remain snow-free most of the year.
American marten may be nocturnal or diurnal. Variability in daily activity patterns has been linked to activity of major prey species, foraging efficiency, gender, reducing exposure to extreme temperatures, season, and timber harvest. In northeastern California, activity in the snow-free season (May–December) was diurnal, while winter activity was largely nocturnal. In south-central Alaska, American marten were nocturnal in autumn, with strong individual variability in diel activity in late winter.
White-tailed ptarmigan males are usually monogamous and remain with the same mate for one breeding season. To attract females, a male will strut and display his tail feathers. The female builds a simple scrape nest on the ground, while the male acts as a sentry to guard the area. The nest is a shallow depression in a snow-free area, generally protected from the wind and is softened with grasses and a few feathers.
Snow line is an umbrella term for different interpretations of the boundary between snow- covered surface and snow-free surface. The definitions of the snow line may have different temporal and spatial focus. In many regions the changing snow line reflect seasonal dynamics. The final height of the snow line in a mountain environment at the end of the melting season is subject to climatic variability, and therefore may be different from year to year.
Location of Robert Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Asemus Beach (, ) is the beach extending 2.2 km on the northwest side of Mitchell Cove in Robert Island in the South Shetland Islands, Antarctica. It is bounded by Debelyanov Point to the southwest, the undulating interior of Alfatar Peninsula to the northwest and Divotino Point to the northeast, and is snow- free in summer.
Bennett Platform () is a high, nearly flat, snow-free mesa of dark rock of Antarctica, about long and wide, located immediately east of Mount Black, on the west side of Shackleton Glacier. It was discovered and photographed by U.S. Navy Operation Highjump (1946–47), on the flights of February 16, 1947, and named by the Advisory Committee on Antarctic Names for Floyd Bennett, copilot on the Byrd North Pole Flight of May 1926.
Location of Snow Island in the South Shetland Islands. Topographic map of Livingston Island, Greenwich, Robert, Snow and Smith Islands. Rebrovo Point (, ‘Nos Rebrovo’ \'nos re-'bro-vo\\) is a point on Aktinia Beach on the southwest coast of Snow Island in the South Shetland Islands, Antarctica projecting 200 m into Boyd Strait. It is situated 2.8 km southeast of Monroe Point and 2.8 km northwest of Cape Conway, and is snow-free in summer.
Winter temperatures rarely rise above freezing, and can be extremely cold, often falling far below zero, especially at night. The top of the mesa is usually snow-free from late June through early October; however, the mesa receives heavy snowfall in the winter, rendering the forest service roads impassable. Accumulations of 20 or 30 inches of snow in the winter are typical. Surrounding areas with lower elevation are warmer and more arid throughout the year.
Adams Glacier descends from the summit ice cap near the center of this view from the northwest. Campgrounds near Mount Adams are open during the snow-free months of summer. Campgrounds in the area include the Takhlakh Lake Campground, offering views across the lake of Mount Adams; Olallie Lake; Horseshoe Lake; Killen Creek; Council Lake; and Keenes Horse Camp. Adams Fork Campground and Twin Falls Campground are located along the Lewis and Cispus Rivers.
In March and April the choughs frequent villages at valley tops or forage in snow-free patches prior to their return to the high meadows. Feeding trips may cover distance and in altitude. In the Alps, the development of skiing above has enabled more birds to remain at high levels in winter. Where their ranges overlap, the two chough species may feed together in the summer, although there is only limited competition for food.
Powder surfing, also known as powsurfing and often spelled as one word e.g. "powdersurfing", is the act of surfing on snow free of any form of bindings and without the aid of ropes, hooks or bungee cords. Powdersurfing is performed on "powsurfer" which is a specially designed board engineered to be controlled using only the rider's feet and balance. This birth of style of riding was inspired by powder snowboarding, surfing and skateboarding.
William Scoresby Bay is a coastal embayment at the western side of William Scoresby Archipelago, Antarctica. It is long and wide, with shores marked by steep rock headlands and snow-free hills rising to 210 m. The practical limits of the bay are extended northward, from the coast by island groups located along its east and west margin. Discovered in February 1936 by Discovery Investigations (DI) personnel on the RSS William Scoresby, for which the bay was named.
The Yukon Telegraph Trail of 1890s fame is still passable through Hatin Lake and provides an overland route to the shield volcano. Alternatively, fixed-wing aircraft landings can be made on a runway at Sheslay. Charter helicopter service in the small community of Dease Lake provides direct access to the Level Mountain Range. The alpine lava plateau of Level Mountain is easily travelled by horse or on foot during the snow free period from June to September.
Binary Peaks is a steep pinnacle covered with snow with two snow free and therefore conspicuous summits, situated northwest of Mount Krokisius and north-northwest of Moltke Harbor, South Georgia. This feature was named "Doppelspitz" (double peaks) by a German expedition under K. Schrader, 1882–83, and was identified by the British Combined Services Expedition of 1964–65. An English form of the name, Binary Peaks, was recommended by the UK Antarctic Place-Names Committee in 1971.
Lester Peak () is a prominent snow-free peak at the south side of Hyde Glacier 1 nautical mile (2 km) northeast of Buggisch Peak in the Edson Hills of the Heritage Range, Marie Byrd Land, Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos from 1961–66, and was named by the Advisory Committee on Antarctic Names for Lester A. Johnson, a meteorologist at Little America V Station in 1958.
The rivers Amur, Sungari, Nonni, Mutang-Kiang, Ussuri, Liao, Yalu and Tumen, and the lakes Khanka, Buir-Nor and Hulun-Nor are all important fish sources. Species include trout, salmon, and European perch. With the exception of Buir- Nor and Hulun-Nor, these can be fished only in snow-free months. The latter lakes are useful fish sources for residents in Xing'an Province near the Russian-Mongolia frontier area, and were a cause of frontier disputes.
In the Sydney region, some birds appear to move down from the Blue Mountains to Sydney for the cooler months, yet others remain in either location for the whole year. It is only seen in alpine and subalpine areas of the Snowy Mountains in warmer snow-free months (mainly October to April). Other populations of crescent honeyeaters follow a more nomadic pattern of following food sources; this has been recorded in the Blue Mountains and parts of Victoria.
Occasionally snow can be seen to lie towards the Chilterns while central London is snow-free. Typically the warmest day of the year at Hampstead will average with around 14 days in total achieving a value of or higher. The average coldest night should fall to . On average 35.8 nights will report an air frost, some 119 days of the year will register at least 1mm of precipitation, and on 7.4 days a cover of snow will be observed.
In sunny weather the mountain can be climbed to within about 2-3 rope lengths of the summit on the often snow-free south face. After an anchor broke causing a roped team to fall with the loss of three lives, all frequently used south face routes were equipped with climbing bolts. The easiest one is the normal south face route (IV). Two abseil pistes (100 metres) run back to the foot of the south face.
A nunatak is a type of glacial refugia that is located on the snow-free, exposed peaks of mountains, which lie above the ice sheet during glaciations. The identification of ‘diversity hotspots’ in areas, which should have been migration regions during major glacial episodes, is evidence for nunatak glacial refugia. For example, the Monte Rosa mountain ranges, the Avers, and the Engadine and the Bernina are all floristically rich proposed nunatak regions, which are indicative nunatak glacial survival.
US Forest Service Fire Ecology It grows in windy, exposed, snow-free rock outcrops on mountain peaks in several ranges, including the Cascade Range and the Front Range of the Rocky Mountains. It is most common on dry soils in open areas, tolerating desiccation relatively easily. This lycophyte forms mats or cushions of creeping stems which fork into small, upright branches. The green, linear or lance-shaped leaves are up to 5 millimeters long including the short, soft bristles on the tips.
Fossil Bluff hut sits at the foot of a scree-covered ridge overlooking George VI Sound which separates mountainous Alexander Island from Palmer Land. George VI Ice Shelf occupies the sound and provides a north-south route for travelling parties except in high summer when the ice shelf's surface is flooded with meltwater. To the west and north-west lie Planet Heights, an extensive range of mountains rising to over . Immediately to the west lies Giza Peak and the snow-free Promenade Screes.
"Matanuska" is derived from the Russian term for the "copper river people".Dictionary of Alaska Place Names, Donald J. Orth author, United States Government Printing Office (1967), page 628 The Matanuska Peak Trail is a five mile one-way hike with 5,670 feet of elevation gain and minor scrambling. The months June through October offer the most favorable weather and snow-free trail conditions to climb this peak. The Matanuska Peak Challenge is a strenuous race run in August each year.
The snow-free debris hills around the lagoon are lateral and terminal moraines of a valley glacier in Nepal. A moraine is any glacially formed accumulation of unconsolidated glacial debris (regolith and rock) that occurs in both currently and formerly glaciated regions on Earth (i.e. a past glacial maximum), through geomorphological processes. Moraines are formed from debris previously carried along by a glacier, and normally consist of somewhat rounded particles ranging in size from large boulders to minute glacial flour.
The Lilliput Nunataks () are three nunataks, from high and trending southeast–northwest, located north of Gulliver Nunatak on the east side of Graham Land, Antarctica. The nunataks are snow free on their southeast sides. They were charted by the Falkland Islands Dependencies Survey and photographed from the air by the Ronne Antarctic Research Expedition in 1947. The name, from Jonathan Swift's Gulliver's Travels, means land of small people and was applied by the UK Antarctic Place-Names Committee in association with Gulliver Nunatak.
Analysis of Ben Nevis's snow is not as comprehensive as that of the Cairngorms, but recent observations show that Ben Nevis has been snow-free only once since 2006 (in 2017). The largest patch, at Observatory Gully, sits at an altitude of around . The slightly lower patch at Point 5 gully has also been known to survive from one winter to the next. Aonach Mòr has a corrie known to hold snow from one year to the next: Coire an Lochain.
Location of Ioannes Paulus II Peninsula on Livingston Island in the South Shetland Islands Topographic map of Livingston Island and Smith Island Gerlovo Beach (, ) is a beach extending 2 km on the northwest coast of Ioannes Paulus II Peninsula on Livingston Island in the South Shetland Islands, Antarctica. It stretches both south and northeast of Mercury Bluff, facing San Telmo Island to the north by west, and featuring Belomortsi Point in its northern part. Snow-free in summer, with area ca. .L.L. Ivanov.
Satellite image of Switzerland in October 2002. On the north side of the Alps, the regions located above 2000m are covered by snow. The canton of Ticino (on the south side) is almost snow-free in early autumn. The Alpine region of Switzerland, conventionally referred to as the Swiss Alps (, , , ), represents a major natural feature of the country and is, along with the Swiss Plateau and the Swiss portion of the Jura Mountains, one of its three main physiographic regions.
The Jawahar Tunnel is a long tunnel through Pir Panjal mountain under the Banihal pass connects Banihal with Qazigund on the other side of the mountain. The Jawahar Tunnel was named after the first Prime Minister of India was constructed in early 1950s and commissioned in December 1956 to ensure snow- free passage throughout the year. It is at elevation of about . It was designed for 150 vehicles per day but now used by more than 7,000 vehicles per day.
Later in the summer there is more travel on talus (scree) and more danger from rockfall. An alternative in snow-free conditions is to hike up to the saddle between the peak and Hagerman Peak. From that point there are climbers' trails which proceed on the opposite (west) side of the ridge to the summit. A different and much less used route climbs the west side of Snowmass Mountain from Geneva Lake, which is accessed from the North Fork of the Crystal River.
A broad area of low pressure brought snow to parts of the Southeast beginning on February 19, when snow began to fall in the mountains of Tennessee. 4.2 and 4 inches of snow accumulated in Waynesville and Mount LeConte respectively. Similar but slightly lesser amounts occurred in surrounding areas of Eastern Tennessee and Western North Carolina. Another swath of snow occurred in Eastern North Carolina and Southeastern Virginia on February 20–21, ending a 400+ day snow- free streak in the region.
Because lateral moraines are deposited on top of the glacier, they do not experience the postglacial erosion of the valley floor and therefore, as the glacier melts, lateral moraines are usually preserved as high ridges. Moraines clearly seen on a side glacier of the Gorner Glacier, Zermatt, Switzerland. The lateral moraine is the high snow-free bank of debris in the top left hand quarter of the picture. The medial moraine is the double line of debris running down the centre-line of the glacier.
By 12 October, snow cover across Northern Parts of Scandinavia had mainly melted, but snow cover across far east and north Russia become much more widespread. By the 17th, snow cover, although patchy, had advanced into central western Russia, with most of Scandinavia snow free again. By the 26th, the first snow cover started to appear of the United Kingdom and more general snow cover over most of Russia and Scandinavia. By 26 November, most of Russia was snow covered as well as Scandinavia.
Egg, Collection Museum Wiesbaden The first thing buff-bellied pipits do when they arrive on the breeding site, during snowmelt, is pairing. Indeed, males will start to fight one on one to win over the female and pair with it during the entire breeding season. They also fight for the snow-free sites that would be better for nesting. The moment is also very important because the melting snow implies an increase in arthropods abundance, which constitute the main food source for these birds.
Climbing the Narrows in Sentinel Rock Rock climbing is an important part of Yosemite. In particular Yosemite Valley, which is surrounded by famous summits like Half Dome and El Capitan. Camp 4, a walk-in campground in the Valley, was instrumental in the development of rock climbing as a sport, and is listed on the National Register of Historic Places. Climbers can generally be spotted in the snow-free months on anything from ten-foot-high (3 m) boulders to the face of El Capitan.
Snowcoaches are a popular mode of transportation for tourists in areas such as Yellowstone Park in the United States and the Columbia Icefield situated in Jasper National Park, Canada. Snowcoaches can be outfitted with either a rubber track or a ski system (replacing tires). Often called by the brand name Mattracks, these rubber track systems can travel over thinner snow depths and even bare road patches without tearing up roadways. Metal-based ski systems can cause more damage or get stuck when traveling over snow-free patches.
Often snow can be seen to lie on the North Downs near Croydon when central London is snow free. The record high temperature at Greenwich is recorded during August 2003. Sunshine is notably lower than other London area weather stations (by about 50–100 hours a year), suggesting Greenwich may be a fog trap in winter, and that the hillier land to the south may obscure early morning and late evening sunshine. The highest temperature recorded across south London was on the same occasion at Kew Gardens.
Parturition timing for northern alpine herbivores is vital due to the brief snow-free timeframe and lack of food sources. The parturition time of most collared pikas is often synchronous in terms of breeding, however there has been a study that has identified some correlation between variation in initiating the first litter and the variation of timing of the snowmelt. Upon finding some asynchronous breeding among pikas, due to not being able to predict snowmelt, this type of breeding could ensure some success in breeding.
Tethys Nunataks () is a minor group of about five snow-free nunataks, lying 2 nautical miles (3.7 km) northeast of Stephenson Nunatak in the southeast corner of Alexander Island, Antarctica. Presumably first seen by Ronne and Eklund of the United States Antarctic Service who sledged through George VI Sound in 1940–41. Surveyed in 1949 by the Falkland Islands Dependencies Survey and named by the United Kingdom Antarctic Place-Names Committee for association with nearby Saturn Glacier, Tethys being one of the satellites of the planet Saturn, the sixth planet of the Solar System.
It was located on ice and used only during the summer. After a few years, it was so covered in snow that it was not possible to dig out. When searching for a new station, the Norwegian Polar Institute decided to find an area which would be snow-free in January and February and which was close to blue ice that would allow the establishment of an airfield. The area was explored by helicopter on January 11, 1990 and the expedition decided to establish a base on the lower parts of Jutulessen.
A tunnel at elevation of through Pir Panjal mountain under the Banihal pass connects Banihal with Qazigund on the other side of the mountain. The tunnel named Jawahar tunnel after the first Prime Minister of India was constructed in early 1950s and commissioned in December 1956 to ensure snow-free passage throughout the year. However, it remains closed for a few weeks in winter due to snow avalanches. It was designed for 150 vehicles per day in either direction but now used by more than 7,000 vehicles per day in both directions.
Four dots are used for broken lines on freeways, and broken lines on surface streets may use only three dots. Reflective pavement markers are placed at regular intervals between Botts' dots to increase the visibility of lane markings at night. In the Las Vegas area of southern Nevada, roads with multiple lanes use four pavement markers for each broken white line, a reflective marker followed by three Botts' dots. More recently, Botts' dots have been used in the snow-free areas of Alabama, Florida, Hawaii, Louisiana, Mississippi, Nevada, Georgia, Washington, and Texas.
Cobalescou Island or Cobălcescu Island is a small snow-free island with two rounded summits, lying east-southeast of Veyka Point, the south extremity of Two Hummock Island in the Palmer Archipelago, Antarctica. The island was discovered and named by the Belgian Antarctic Expedition under Gerlache, 1897–99.Cobalescou Island, at the Composite Antarctic Gazetteer The established name appears to be a corrupted spelling. The toponym was suggested to Gerlache by Emil Racovitza, Romanian zoologist and botanist of the Belgian Antarctic Expedition, for Romanian scholar Grigore Cobălcescu, a geologist of European reputation.
The climate is mild, with mostly snow-free winters, and warm summers. The island probably gained its name because the soil consists mostly of sand. To maintain a garden, it is in many places necessary to enrich the soil with seaweed. Though the island is in no way self-sufficient, with most of the adult residents working on the mainland, it manages to maintain a strong community, with a school, a kindergarten, a movie theater, a choir, a local store, a boat building workshop, and an architect's office.
The expedition discovered the existence of the only snow-free Antarctic valleys, which contain Antarctica's longest river. Further achievements included the discoveries of the Cape Crozier emperor penguin colony, King Edward VII Land, and the Polar Plateau (via the western mountains route) on which the South Pole is located. The expedition tried to reach the South Pole travelling as far as the Farthest South mark at a reported 82°17′S. As a trailbreaker for later ventures, the Discovery Expedition was a landmark in British Antarctic exploration history.
The best time is in January and March, where the approach is snow free, except for some specific areas, and the climate is more stable. The Incas climbed to its summit periodically in the 15th century. The first European ascent of the mountain was by Gustav Brandt and Rudolph Lucke in 1896. During a flight from Santiago, Chile, to Mendoza, Argentina, on 16 July 1932, the Pan American-Grace Airways (Panagra) Ford Trimotor San José crashed on Cerro El Plomo during a severe snowstorm, killing all nine people on board.
Tree trunks absorbing sunlight become warmer than the air and cause earlier melting of snow around them. The snow does not melt slower gradually with distance from the trunk, but creates a wall surrounding snow-free ground around it rather. According to some of sources, North American spring ephermal plants like spring beauty (Claytonia caroliniana), trout lily (Erythronium americanum) and red trillium (Trillium erectum L.) benefit from such thaw circle. They can emerge earlier inside these circles, what gives them more time before development of tree canopy foliage cutting off significant portion of the light.
Mount Dolber () is a prominent mountain, high, with a large snow-free summit, located between Mount Rea and Mount Cooper in the Sarnoff Mountains, Ford Ranges, Marie Byrd Land. It was mapped by the United States Antarctic Service (1939–41) and by the United States Geological Survey from surveys and U.S. Navy air photos (1959–65). It was named by the Advisory Committee on Antarctic Names for Captain Sumner R. Dolber, United States Coast Guard, captain of the icebreaker Southwind in the Antarctic Peninsula Ship Group (1967–68) and the Ross Sea Ship Group (1968–69).
Troll is a Norwegian research station located at Jutulsessen, from the coast in the eastern part of Princess Martha Coast in Queen Maud Land, Antarctica. It is Norway's only all-year research station in Antarctica, and is supplemented by the summer-only station Tor. Troll is operated by the Norwegian Polar Institute and also features facilities for the Norwegian Meteorological Institute and the Norwegian Institute for Air Research. Contrary to most other research stations on the continent, Troll is constructed on the snow-free slope of solid rock breaking through the ice sheet at Jutulsessen, located above mean sea level.
Montrose is also the location of the "Antenna Trail" a 4 kilometre loop hiking trail that rises 250 metres above the village and has views of the Beaver and Columbia Valleys. This trail is part of the Kootenay Columbia Trail system although it is not contiguous with the rest of the trails located near, and accessed from, nearby Rossland. The Antenna Trail is popular because it is snow-free much earlier in the spring than the higher elevation trails, and has little if any mountain bike traffic. The village shares its territory with a variety of native BC wildlife.
The Keeskogel, a mountain with a height of , lies in the Venediger Group of the High Tauern in Austria. The summit is located about 4 km as the crow flies northwest of the Großvenediger (). The waymarked, glacier-free normal route from the Kürsinger Hut (), is a relatively straightforward climb in dry and snow-free condition and takes about 1½ to 2 hours to reach the summit (sure- footedness required). Especially impressive in good weather is the view from the summit of the north side of the Großvenediger and the main chain of the Tauern and the glaciated landscape of the Obersulzbachkees and Untersulzbachkees.
Japan deployed cyclists to great effect in its 1941 to 1942 campaign in Malaya and drive on Singapore during World War II. A horsed cavalry regiment of the Philippine Scouts assisted in the defense of the Philippines at the onset of World War II. The 10th Mountain Division of the U.S. Army also maintained a Mounted Reconnaissance Troop throughout World War Two, which saw service in Italy and Austria during the war. Countries with entrenched military traditions, such as Switzerland, retained horse-mounted troops well into the Cold War, while Sweden kept much of its infantry on bicycles during the snow-free months.
On the descent of the glacier Scott and Evans survived a potentially fatal fall into a crevasse, before the discovery of a snow-free area or dry valley, a rare Antarctic phenomenon. Lashly described the dry valley as "a splendid place for growing spuds". The party reached Discovery on 24 December, after a round trip of seven hundred miles covered in 59 days. Their daily average of over 14 miles on this man-hauling journey was significantly better than that achieved with dogs on the previous season's southern journey, a fact which further strengthened Scott's prejudices against dogs.
These included the snow-free Dry Valleys in the western mountains, the emperor penguin colony at Cape Crozier, scientific evidence that the Ice Barrier was a floating ice shelf, and a leaf fossil discovered by Ferrar which helped to establish Antarctica's relation to the Gondwana super-continent. Thousands of geological and biological specimens had been collected and new marine species identified. The location of the South Magnetic Pole had been calculated with reasonable accuracy. On the medical side, Wilson discovered the anti-scorbutic effects of fresh seal meat, which resolved the lethal threat of scurvy to this and subsequent expeditions.
A study began in 2009 regarding the feasibility of a road from Hoonah to Pelican and possibly connecting to Tenakee Springs to allow an energy corridor to hot spring thermal energy sources in the region for Hoonah, to lower heating and energy costs. Most Tenakee residents expressed opposition to the road, while Pelican has generally supported the idea. The road would save the Alaska Department of Transportation ferry costs in summer snow-free months, by connecting these areas to Hoonah. According to the United States Census Bureau, the city of Hoonah has a total area of , of which are land and , or 17.59%, are water.
The northern boundary of its occurrence commenced on the coast of the Sea of Japan at 44°N and ran south at a distance of from the coast to 43°10'N. There its range turned steeply westward, north of the Suchan River basin, then north to encompass the source of the Ussuri River and two right bank tributaries in the upper reaches of the Ussuri, and westward toward the bank of Khanka Lake. In the 1950s, leopards were observed north of Vladivostok and in Kedrovaya Pad Nature Reserve. The association of the leopard with mountains is fairly definite, and to snow-free south-facing rocky slopes in winter.
The Blackwall Mountains () in Antarctica rise to , extending in a west- northwest–east-southeast direction for and lying close south of Neny Fjord on the west coast of Graham Land. They are bounded to the east by Remus Glacier, to the south by Romulus Glacier, and are separated from Red Rock Ridge to the west by Safety Col. First roughly surveyed in 1936 by the British Graham Land Expedition under John Rymill, they were re-surveyed in 1948–49 by the Falkland Islands Dependencies Survey, and so named by them because the black cliffs of the mountains facing Rymill Bay remain snow free throughout the year.
Location of Greenwich Island in the South Shetland Islands The southern part of Kladara Beach from Shopski Cove, with Provadiya Hook in the foreground Topographic map of Livingston Island and Smith Island Kladara Beach (, ) is the 2 km beach forming the south side of Yankee Harbour on the southwest coast of Greenwich Island in the South Shetland Islands, Antarctica. Bounded by the base of Provadiya Hook to the west, Oborishte Ridge to the south, and the terminus of Solis Glacier to the east. It is snow-free in summer. The beach is named after the ancient and medieval fortress of Kladara in Southeastern Bulgaria.
The Gilman Glacier is one of the largest glaciers draining into Lake Hazen. To the est, the mountain range extends across the Hazen Plateau while, to the west, it runs virtually to the head of Tanquary Fiord. The mountains, which tower as much as above Lake Hazen, typically consists of steep snow-free slopes facing south, with north-facing slopes of shallow gradients covered in snow and ice. At intervals, the range is bisected by broad valleys in width that are occasionally filled by glacial tongues, such as the monumental Henrieta Nesmith Glacier that descends to within of Lake Hazen near its northwestern end.
Map of the McMurdo Sound and the Dry Valleys Location of valleys (indicated by red dot) within the Ross Dependency The McMurdo Dry Valleys are a row of largely snow-free valleys in Antarctica, located within Victoria Land west of McMurdo Sound. The Dry Valleys experience extremely low humidity and surrounding mountains prevent the flow of ice from nearby glaciers. The rocks here are granites and gneisses, and glacial tills dot this bedrock landscape, with loose gravel covering the ground. The region is one of the world's most extreme deserts, and includes many features including Lake Vida, a saline lake, and the Onyx River, a meltwater stream and Antarctica's longest river.
Joseph started conservatively in this sector, selling railroad bonds, but this led them to owning and operating railroads in order to protect their investments. Joseph served as director of the A&P;, the Missouri–Kansas–Texas, as well as the South Pacific railroads, and in 1872, claimed that they had made a fortune in the business of start-up railroads. However, he never felt comfortable here, and suspected that they were over-invested in the sector. After the Panic of 1873 he swore never to sell another railroad bond, but in 1874 was again selling A&P; bonds, touted as the only snow-free route to the Pacific.
Botts' dots had also been employed previously in Albuquerque, but the city has since discontinued their use in favor of reflective paint for pavement markings. Until the late 1990s, Botts' dots were also used extensively in the snow-free areas of Arizona, however, ADOT has since ended this practice, opting for painted stripes with reflective markers instead. However, they can still be found on US Route 95 south of Yuma, as well as on some local streets in Yuma and Tucson. Many states in snow-prone areas of the Midwest and Northeastern United States use reflectors placed into protective metal castings, which allow them to be plowed over without being dislodged from the road surface.
Clemens Bro made Søndergade into the premier commercial street in the city, connecting the old neighborhoods north of the river to the newer developments, such as Frederiksbjerg, south of the river. Several buildings constructed in the 1850s were demolished in favor of larger structures that could accommodate the need for larger businesses. In 1904 The first electrical tram lines were built to run through Ryesgade and Søndergade and in 1929 it was widened to a double line. In 1972, on 7 November, Søndergade was pedestrianized, the tram lines removed and new paving stones, street lights, benches, trees and phone booths put in while heating was installed under the street to keep it snow-free during winter.
This region has cool wet winters, and hot dry summers, with rainfall decreasing and summer temperatures increasing with distance from the sea. The region ranges from Pemberton, located in the Karri Forest region of the extreme southwest corner of the state has an average rainfall of 1244 mm over 167 days, to Bencubbin in the northeast wheat belt with only 319 mm over 73 days. Coastal regions are generally free from frosts, although frost conditions on winter nights are not uncommon. The state is generally snow free throughout winter, although an occasional fall is reported once or twice a year on the Stirlings or Porongurups north of Albany (837 mm over 179 days).
Mojave Road Plaque The land was taken from Mexico by the US in 1848 following the Mexican–American War. In early 1858 the Mohave Trail became the Mojave Road, a wagon road connected to the newly pioneered Beale's Wagon Road across northern New Mexico Territory from Fort Defiance to Beale's Crossing on the Colorado River where it linked up with the Mojave Road. Wagon trains of settlers coming west on the Santa Fe Trail soon followed Beale's Wagon Road and the Mojave Road into Southern California. Beale's road was shorter than the route via the more southern Southern Emigrant Trail and it was cooler in summer, snow-free in winter, had better forage, and was better watered.
By the fall of 1975, melting of Sherman Crater glacier resulted in a snow-free area three times larger than typical summer exposure and revealed a shallow crater lake and previously unknown fumaroles. Sampling fumarole gas at Sherman Crater in 1981 A major concern was that an eruption might cause the walls of Sherman Crater to collapse, sending lahars into Baker Lake reservoir and cause a wave to overtop, or significantly damage, the Upper Baker Dam. Either event would result in a large volume of water rushing into the Lake Shannon reservoir and potentially cause a surge of water over, or failure of, the Lower Baker Dam. Failure of the Lower Baker Dam would result in catastrophic flooding down the Skagit River with little to no warning.
Stillwell Hills is a group of largely snow-free rocky hills composed of banded gneisses and including Kemp Peak and Lealand Bluff, extending along the southwest side of William Scoresby Bay. This area was explored by Discovery Investigations personnel on the RSS William Scoresby in February 1936, and by the Lars Christensen Expedition, 1936–37, the latter group taking air photos used to map these hills for the first time. Geologic investigation of the area was made by Australian National Antarctic Research Expeditions (ANARE) in 1961. Named by ANCA for Dr. Frank Leslie Stillwell, geologist with Australasian Antarctic Expedition (AAE), 1911–14, who derived a theory of metamorphic differentiation from banded gneisses of the same type on George V Coast.
The expedition's Arctic tents were pitched for the first time at Shekar, to general approval, and a hair- cutting session took place, Wyn-Harris proving a capable barber. On 13 April the party departed, crossing the 17,000 ft Pang La before the descent to Tashidzom, where the expedition's ponies were stabled. Chö-Dzong was reached on 15 April, from a hill above which a clear view of Mount Everest was obtained with a naval telescope. The north face appeared relatively snow-free and the ledges along which Norton traversed were clear to the eye but, according to Ruttledge, looking "remarkably difficult", while the overhanging Second Step appeared "a formidable obstacle" and, although the summit slopes looked feasible, "the problem was to reach [them] across the frightful slabs of the couloir walls".
Route of the Old Spanish Trail from Santa Fe to Los Angeles. The first large use of the route pioneered by Hunt and the Veterans were hundreds of late arriving Forty-niners, and some parties of Mormons, both packers and teamsters, looking to avoid the fate of the Donner Party, by using this snow free route into California in the fall and winter of 1849 - 1850. From Parowan onward to the southwest, the original route closely followed the route of the Old Spanish Trail diverting from that route between the Virgin River at Halfway Wash to Resting Springs, following the cutoff discovered by John Freemont on his return from California in 1844. This road only diverted to find places that could be traversed by the wagons of Mormon and Forty-niner parties that pioneered it.
Hundreds of late arriving Forty-niners, and some parties of Mormons, both packers and teamsters, looking to avoid the fate of the Donner Party, in the fall and winter of 1849–1850 used the snow free Southern Route to Southern California. This route, that ran southwest from Salt Lake City, was pioneered by Jefferson Hunt in 1847–48 and a party of veterans of the Mormon Battalion returning from California in 1848. From Parowan onward to the southwest, the original route closely followed the route of the Old Spanish Trail diverting from that route between the Virgin River at Halfway Wash to Resting Springs, following the cutoff discovered by John Freemont on his return from California in 1844. This road only diverted to find places that could be traversed by the wagons of Mormon and Forty-niner parties that pioneered it.
In January 2008, the Norwegian newspaper Aftenposten estimated that some 13,000 moose had died in collisions with Norwegian trains since 2000. The state agency in charge of railroad infrastructure (Jernbaneverket) plans to spend 80 million Norwegian kroner to reduce collision rate in the future by fencing the railways, clearing vegetation from near the tracks, and providing alternative snow-free feeding places for the animals elsewhere. In the Canadian province of New Brunswick, collisions between automobiles and moose are frequent enough that all new highways have fences to prevent moose from accessing the road, as has long been done in Finland, Norway, and Sweden. A demonstration project, Highway 7 between Fredericton and Saint John, which has one of the highest frequencies of moose collisions in the province, did not have these fences until 2008, although it was and continues to be extremely well signed.
A heated sidewalk in Holland, Michigan Installation of under-floor heating in Reykjavík, Iceland Heat mats A snowmelt system prevents the build-up of snow and ice on cycleways, walkways, patios and roadways, or more economically, only a portion of the area such as a pair of -wide tire tracks on a driveway or a center portion of a sidewalk, etc. It is also used to keep entire driveways and patios snow free in snow prone climates. The "snow melt" system is designed to function during a storm thus improve safety and eliminate winter maintenance labor including shoveling or plowing snow and spreading de- icing salt or traction grit (sand). A snowmelt system may extend the life of the concrete, asphalt or under pavers by eliminating the use of salts or other de-icing chemicals, and physical damage from winter service vehicles.
During snowfalls when temperatures hover close to freezing, northern parts of the city, such as around Derry Road, including Pearson Airport away from warmer Lake Ontario usually get more snow that sticks to the ground because of the lower temperatures. The reverse occurs when a strong storm approaches from the south kicking up lake effect snow, bringing higher snowfall totals to south Mississauga. The city usually experiences at least six months of snow-free weather; however, there is the odd occurrence where snow does fall either in October or May, none which sticks to the ground. The Port Credit and Lakeview areas have a micro-climate more affected by the proximity of the open lake, warming winter temperatures as a result but it can be sharply cooler on spring and summer afternoons, this can also be the case in Clarkson, but with much less consistency.
Location of Greenwich Island in the South Shetland Islands Topographic map of Livingston Island area featuring Flamingo Beach Flamingo Beach (, ) is the beach on Drake Passage extending 2.6 km in east-west direction and 600 m wide, situated on the north coast of Greenwich Island in the South Shetland Islands, Antarctica. Snow-free in summer, it is bounded by Terimer Point to the west, Orión Passage to the north, Agüedo Point to the east, Quito Glacier to the southeast and Teteven Glacier to the southwest. Proteus Lake is situated in the central part of the beach and Nereid Lake lies near its eastern end. The area was visited by early 19th century sealers. The beach is “named after the ocean fishing trawler Flamingo of the Bulgarian company Ocean Fisheries – Burgas whose ships operated in the waters of South Georgia, Kerguelen, the South Orkney Islands, South Shetland Islands and Antarctic Peninsula from 1970 to the early 1990s.
Transport in Antarctica takes place by air, using fixed-wing aircraft and helicopters. Runways and helicopter pads have to be kept snow free to ensure safe take off and landing conditions. Antarctica has 20 airports, but there are no developed public-access airports or landing facilities. Thirty stations, operated by 16 national governments party to the Antarctic Treaty, have landing facilities for either helicopters and/or fixed- wing aircraft; commercial enterprises operate two additional air facilities. Helicopter pads are available at 27 stations; runways at 15 locations are gravel, sea-ice, blue-ice, or compacted snow suitable for landing wheeled, fixed-wing aircraft; of these, one is greater than 3 km in length, six are between 2 km and 3 km in length, 3 are between 1 km and 2 km in length, three are less than 1 km in length, and two are of unknown length; snow surface skiways, limited to use by ski-equipped, fixed-wing aircraft, are available at another 15 locations; of these, four are greater than 3 km in length, three are between 2 km and 3 km in length, two are between 1 km and 2 km in length, two are less than 1 km in length, and data is unavailable for the remaining four.

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