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"hogback" Definitions
  1. a ridge of land formed by the outcropping edges of tilted strata
"hogback" Synonyms
hogframe hogging frame hill mound elevation rise eminence height upland hump prominence ridge hillock highland hummock mount cliff knoll bank tor precipice altitudes crest panache caruncle crown cockscomb comb chine growth More
"hogback" Antonyms
hollow valley dale dene vale combe dell dingle glen slade bottom clough strath

202 Sentences With "hogback"

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

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The source continued that the Type 094 had a "weird hogback" design based on the old Soviet Delta class nuclear submarines to get round space constraints that limited its missile capacity.
Hogback is a mountain in Schoharie County, New York. It is located northeast of Cobleskill. Barrack Zourie is located northwest and Mount Shank is located southwest of Hogback.
Waterflow is located at .googlemaps Waterflow is a high desert valley with the highest point being a geological hogback called "Hogback". The San Juan River and Shumway Arroyo are important water resources in the area.
Hogback Mountain or Hogsback Mountain is a large hill northeast of Klamath Falls, Oregon, United States. Hogback was named because from Klamath Falls, the hill looks similar to the shoulders of a pig. The majority of Hogback is privately owned, but open to hikers. Fence tampering and all-terrain vehicle (ATV) use is strictly prohibited due to livestock activities on the mountain and surrounding areas.
The hogback is significant because it marks part of the boundary between the Colorado Plateau to the west and the Southern Rocky Mountains to the east.Colorado Mountain College. The Grand Hogback: Living life on the edge. Retrieved: March 27, 2017.
Brushy Mountain and Hogback Mountain are principal ridges in the cluster. Brushy Mountain, one of the broad ridges composing the Ridge and Valley formation, is capped by Mississippian Price sandstone. Hogback Mountain is another ridge running parallel to Brushy Mountain on the west.
View of the city from Dinosaur Park Skyline Drive follows the summits of the Dakota Hogback south from near Rapid Gap (where Rapid Creek cuts through the Hogback) to a large high plateau that forms the current south edge of Rapid City. The Central and Eastern portions of Rapid City lie in the wide valley of Rapid Creek outside the Hogback. It includes a number of mesas rising a hundred feet or more above the floodplain.
A Viking Age hogback in Sockburn, County Durham, North East England may depict Týr and Fenrir.McKinnell (2005:16).
Hogback Mountain is a mountain in southern Vermont, United States, in the town of Marlboro, Vermont, just north of Vermont Route 9. Its main peak is high. The area is well known for expansive views from Route 9. Hogback Mountain Ski Area was located across Route 9 on Mount Olga.
St Kentigern's Church Aspatria, Hogback A Hogback is a recumbent coped shrine tombstone, shaped to represent the house of the dead, with a roof carved to look like tiles, and walls carved to represent ideas symbolic with death and resurrection.Bailey page 18 When the builders dismantled the old Norman church they found a Hogback in the building material. It is 1.17 metres long and 69 centimetres high. At the top is a highly decorated ridge, 7.6 centimetres thick, with two zigzag flat bands worked upon it.
The hogback tombstone displayed now in Brechin Cathedral is an eleventh-century stone carving in the Norse Ringerike style. Though one end of the hogback has been damaged, the remainder displays relief carvings of clerics intertwined with animals and the head of a large-eyed beast. Foliage is carved across the top.
In the church are a number of ancient stones, one of which is known as the Hogback stone. This dates from the early 11th century, the name Hogback referring to its curving shape. It consists of hard grey sandstone, not a type of stone found locally. There is a ring of eight bells.
In the case of the Brechin Hogback, the figures are carrying objects that are characteristic of early medieval Irish monasticism.
Monoclinal slopes mimic the structural form of monoclines whereas monoclinal hogback ridges form on the steep eroded slope of monoclines.
A new interchange east of the western terminus was added at Hogback Road in Luther, and was opened in May 2011.
The Grand Hogback Monocline defines the eastern limit of the Uinta-Piceance Basin The Grand Hogback is a 70-mile long,New Castle, Colorado. Living in New Castle. Retrieved: March 27, 2017. curving, spine-like ridge in Western Colorado that extends from near McClure Pass in Pitkin County through Garfield County and then to near Meeker in Rio Blanco County.
Based on the Köppen climate classification, Hogback Ridge is located in a subarctic climate zone with long, cold, snowy winters, and cool summers. Temperatures can drop below −20 °C with wind chill factors below −30 °C. This climate supports the Corbin, Keystone, and Hogback Glaciers on the mountain. The months May through June offer the most favorable weather for viewing and climbing.
The four primary landscape styles produced in nearly flat-lying sedimentary layers are bench-and-slope landscape, erosional mountains, monoclinal slopes, and monoclinal hogback ridges.
Oil is produced from the Niobrara in the North Park Basin, and new fracturing methods are allowing much larger areas to be tapped for oil.Google article The Fort Hays member was historically mined on the High Plains for the manufacture of Portland cement at Superior, Nebraska and Yocemento, Kansas, as well as along the Dakota Hogback in Colorado from Lyons to Boulder, and around Pueblo and Florence.Kansas Geological Survey: Fort Hays Chalk, accessed 20 January 2009. Along the Dakota Hogback north of Laporte, Colorado, the Fort Hays Limestone formed a secondary hogback, which was extensively quarried for manufacture of up to 450,000 tons of cement a year.AggregateResearch.
In the south chancel aisle is a Viking hogback stone and on the west wall is a medieval sepulchral slab with a floriated cross and sword.
A monocline, the Grand Hogback is part of the Mesaverde Formation. The ridge formed towards the end of the Laramide orogeny during the middle to late Eocene.
See discussion in, for example, Davidson (1993:39–41). A Viking Age hogback in Sockburn, County Durham, North East England may depict Týr and Fenrir.McKinnell (2005:16).
The path through the hogback features a massive cut that exposes various layers of rock millions of years old. The site includes a nature study area for visitors.
The crew of the island-sized ship , captained by Gecko Moriah, consists mostly of zombies, numbering in the hundreds, created from corpses – patched up by Moriah's subordinate, the medical genius – given unlife in the form of shadows stolen using Moriah's Devil Fruit ability. Placed in charge of the zombies are Moriah's other subordinates, "Graveyard" , a man augmented by Hogback with various animal parts and capable of turning himself and anything he touches invisible, and "Ghost Princess" Perona. Among the zombies created by Hogback and Moriah are , a former famous stage actress whom Dr. Hogback was in love with; , a samurai from the Wano Country; , a warthog-like zombie in love with Absalom; and , a giant formerly feared by all.
Mount Shank is a mountain located in the Catskill Mountains of New York northwest of Cobleskill. Hogback is located northeast, and Donats Mountain is located southeast of Mount Shank.
The tubes were then filled with Portland cement concrete to within of the top, the final fill was with brickwork with a top course of granite. The river abuttments were of brick with stone dressing. The fixed spans were long, made of three wrought iron hogback plate girders each, resting on three piers. The swing span was constructed of three hogback wrought iron box girders, each long, each box girder having a thickness of made of plates thick.
Dakota Ridge is bordered to the east by Denver, to the north by Lakewood, and to the south by unincorporated Ken Caryl. It is bordered to the west by the Dakota Hogback, a sharp hogback ridge that to the north near Morrison is known as Dinosaur Ridge. Colorado State Highway 470, part of the beltway around Denver, runs through the western part of the community, leading north to Golden and southeast to Littleton. Downtown Denver is to the northeast.
Hogback Outlier is an Ancestral Puebloan outlier community located northwest of Chaco Culture National Historical Park, New Mexico. The community features a great house, great kiva, and thirty-five small house sites.
At the start of 2015, the group rented a cabin at Horsetooth Reservoir, located in Dakota Hogback ridge, west of Fort Collins, Colorado. The cabin was surrounded by woods.McMahon ed. 2016, p.
Then Burnt, Swamp, Fox, Cole, Susan, Hogback, Bob, Honey, Clay, Hill, Rock, Britt, Old Hatchery, and French creeks. Little River is next, followed by Fordice, Huntley, Cooper, Oak, Clover, Dixon, and Sutherlin creeks.
Hogback Ridge is a glaciated mountain ridge located in the Chugach Mountains, in the U.S. state of Alaska. This landform is situated east of Valdez, west of Thompson Pass, and the Richardson Highway traverses the southern base of the mountain. This feature takes its name from the Hogback Glacier on its northern slopes, and in turn the glacier was named in 1898 by Captain William R. Abercrombie. Abercrombie led an 1898 expedition seeking a route from coastal Alaska to the Klondike.
It operated from 1946 to 1986, using only natural snow, and blamed the cost of insurance for causing it to close.NELSAP: Hogback Mountain Ski Area Roughly was purchased and given to the town of Marlboro as conservation land, known as Hogback Mountain Conservation Area.hogbackvt.org/ Some of the old ski lifts remain on the property, along with various buildings. Trails are semi-clear, as volunteers continue to keep some open and available to cross country skiers, backcountry skiers, hikers, and snowshoers.
The elevation of the ridge ranges from to . The hogback appears as a series of serrated ridges and is easily discernable from Google Maps and other aerial views. It is visible from Interstate 70.
In the areas of Scandinavian settlement in the northeast of England, hogback tombs were created. Scandinavian settlement also resulted in the return of furnished burials under barrows in several instances, for instance at Ingleby in Derbyshire.
Its topography is dominated by rugged canyons that become deeper and narrower in the east. The Hogback and San Pedro Mountains border the slope in the east. Precipitation in the generally arid region rises with elevation..
Because they are gradational in nature, the exact angle of the backslope used to define these landforms is arbitrary and can vary in the scientific literature.Fairbridge, RW (1968) Hogback and Flatiron. In RW Fairbridge, ed., pp.
According to the U.S. Census Bureau, the county has a total area of , of which is land and (1.5%) is water. The highest point is Hogback Mountain in Shenandoah National Park, along the border with Rappahannock County.
The road curves southwest and reaches the summit of North Marshall. Upon reaching the south- facing Range View Overlook, the roadway turns to the west along a winding path, bending southwest The drive passes the Mount Marshall Overlook on the east side, at which point it heads west. Skyline Drive reaches the Hogback Overlook on Hogback Mountain that faces northwest and turns southerly. The roadway heads west and straddles the boundary between Page and Rappahannock counties, coming to Mathews Arm, where a campground and ranger station are located.
Anne married the abstract painter Ernest Briggs in 1960. Arnold and Briggs bought a house and barn in Montville, Maine, in 1961, at the foot of Hogback Mountain. Briggs died in 1984. Anne's long-time companion was the photographer Robert Brooks.
Overview map of the Heber The Heber is a hogback ridge, relatively small in area and up to 313.5 metres high, in the Lower Saxon Hills within the districts of Goslar, Northeim and Hildesheim in the German state of Lower Saxony.
Hogback Hill () is a rounded mountain, high, rising just north of Hjorth Hill and west of Cape Bernacchi, in Victoria Land, Antarctica. It was charted and given this descriptive name by the British Antarctic Expedition, 1910–13, under Robert Falcon Scott.
Rivers have carved out several gaps in the hogback, the most notable being the one the Colorado River has carved out near New Castle, Colorado. Others include Harvey Gap and Rifle Gap,Colorado Parks & Wildlife. Rifle Gap. Retrieved: March 27, 2017.
The Southern Vermont Natural History Museum is a natural history museum, at the Hogback Mountain Scenic Overlook on Route 9 in West Marlboro, Vermont. The museum is surrounded by the Hogback Mountain Conservation Area, over 600 acres of protected forest land, with views of three states. The Museum was established in 1996 around the Luman Ranger Nelson Natural History Collection, one of the largest collections of native birds and mammals in the northeast, with 250 species represented. The museum's founder Ed Metcalfe intended the museum to serve as an educational resource for local communities and visitors to the area.
St Thomas' Church, Brompton by Northallerton St Thomas' Church on High Green is a Grade I listed building dating from the 12th century with additions in the 14th and 15th centuries and a restoration undertaken in 1868. It is reputed to have the largest collection of Hogback sculptures in the United Kingdom. This collection of hogbacks and Viking period crosses that suggest Brompton was the base for a company of stone carvers during that period. It is thought that the Hogback was invented in the Allertonshire area since the Hogbacks at Brompton and Northallerton are amongst the oldest examples.
Between Golden and Morrison, the Dakota hogback is called Dinosaur Ridge and is the site of a dinosaur trackway and dinosaur fossils exposed in the outcrop that are part of a Colorado State Natural Area and Geological Points of Interest. The Lyons and Lykins formations outcrop in a smaller hogback. Farther west, the Fountain Formation outcrops as flatirons and forms the namesake of the Red Rocks Park and Amphitheatre. Here, against the eastern edge of the Rocky Mountain Front range, the Fountain Formation is in nonconformable contact with the Precambrian crystalline rock of the Idaho Springs Formation.
Joseph Anderson noted that: Also on the island is the 12th-century parish church of St Boniface"St Boniface's". Scottish Church Heritage Research. Retrieved 26 August 2013. (recently restored; open in summer) with a carved Norse "hogback" gravestone (probably also 12th century) in the churchyard.
Quinebaug Woods is located within the Lower Worcester Plateau/Eastern Connecticut Upland Ecoregion. Forest covers the entire property. Hemlock is abundant and suppresses understory diversity. A ridgeline of exposed bedrock, also referred to as a “hogback,” is a prominent feature along the western boundary.
Rapid City is located on the eastern edge of the Black Hills, and has developed on each side of the Dakota Hogback. Rapid City's "Westside" is located in the Red Valley between the foothills of the Black Hills proper and the Dakota Hogback, so named for the red Spearfish formation soils and the way the valley completely encircles the Black Hills. Rapid City has expanded into the foothills, with developments having been built on both ridges and in valleys developed, especially in the last 20 years. This arid edge area has a higher risk of wildfire, as shown by the Westberry Trails fire in 1988.
The carving on the Camus Cross shows distinct similarities with those on the Brechin Hogback stone and point to an Irish Ecclesiastical influence. The foliar designs on the north and south edges, originally seen as Ringerike- like (and hence, Scandinavian in origin), consist of tendrils and volutes with "wave-crest" thickening. These features bear closest similarity with Irish insular art of the late tenth century, and the treatment of the symmetrical foliar scroll design on the lower portion of the west face is diagnostically Irish. The full-face figures on the east face are of an identical type to those on the Brechin Hogback.
Hogback Bridge was an historic Pennsylvania (Petit) truss bridge located in Curwensville, Clearfield County, Pennsylvania, United States. It was built in 1893 by the King Bridge Company. Note: This includes It was listed on the National Register of Historic Places in 1988. It is now torn down.
VT 9 and VT 100 run concurrently follow Beaver Brook to their split east of the town center. The highway ascends Hogback Mountain along Beaver Brook to the stream's source. The route passes Molly Stark State Park and enters the town of Marlboro west of the summit.
The Hogback Bridge was originally one of 19 covered bridges in Madison County; there are only six remaining covered bridges in the county. In 1992, the bridge was rehabilitated for the cost of $118,810 ($ today). It was added to the National Register of Historic Places in 1976.
The hogback combines Celtic and Scandinavian motifs, and is the most complex known stone sculpture in the Ringerike style in Scotland. The inscribed St Mary's Stone has a circular border round the central motif of the Virgin and Child which echoes that on the Round Tower.
In the churchyard are two ancient stone crosses and a rare example of a hogback grave dating from Viking times. A. G. Langdon (1896) also records the existence of four more stone crosses in the parish.Langdon, Arthur G. (1896) Old Cornish Crosses. Truro: J. Pollard; pp.
The Kimberling Creek Cluster is a region in the Jefferson National Forest recognized by The Wilderness Society for its diversity of habitats extending along parts of Brushy and Hogback Mountains. Kimberling Creek, with headwaters in the cluster, flows into Big Walker Creek, a tributary of the New River.
In 1891, Mary L. Eldridge and Miss Mary Raymond were sent by the Women’s Home Missionary Society of the Methodist Episcopal Church to build a mission to administer to the spiritual needs of the Navajos in Jewett, known today as Hogback, New Mexico. Mrs. Mary Eldridge Tripp initially opened her cabin in 1896 as a day school for Navajo children. In 1899, a three- bedroom school house opened in Hogback, New Mexico. The school house consisted of three rooms. Two rooms were used as dorms; one for a boy’s side and the other for a girl’s side, the last room which was in the middle of the two rooms was used as the classroom.
Marine invertebrates have been discovered in a limestone and shale member of the Fountain Formation, cropping out on a low hogback in Perry Park. Invertebrates include bryozoans, brachiopods, crinoids, echinoids, and gastropods.Ellis, C.H., 1966, Paleontologic age of the Fountain Formation south of Denver, Colorado: The Mountain Geologist, v. 3, no.
The upper pair of animals have their heads apparently joined together, the lower pair are entwined and each bites the other's tail. Meigle 24 is one of the lost monuments.Ritchie 1997, p.25. It was a small cross-slab. Meigle 25 is a hogback tombstone dating to the late 10th century.
According to the 2010 census, the township has a total area of , of which (or 96.97%) is land and (or 3.00%) is water. Lakes in this township include Bass Lake, Beaverdam Lake, Deep Lake, Grass Lake, Hogback Lake, Howard Lake, Lake Arrowhead, Otter Lake, Pine Canyon Lake, Shallow Lake and Stayner Lake.
They then proceeded to a ridge called Hogback Hill. The Indians attacked Van Campen's advance guard as it arrived at the top of the hill, causing 16 casualties. The advance guard pursued the Indians and killed several of them. On August 29, 1779, the battle between General Sullivan's army and the Indians began.
Murphy Hogback The NPS requires all motorized vehicles including motorbikes be registered, street- legal and operated by licensed drivers only. ATVs, UTVs and OHVs are not permitted. All vehicles and bicycles must remain on the road surface. Pets are not permitted regardless of whether they could be kept inside a vehicle at all times.
This pattern caused the older thrusts to ride on top of the younger thrusts as they moved eastward. The Paris-Willard thrust in Utah was determined to be the oldest thrust in the series using this pattern. The youngest thrust is the Hogback in Wyoming.Hintze, L., 2005, Utah’s Spectacular Geology, Department of Geology, Brigham Young University, pp.
The drive sits on the top of Skyline Ridge, a hogback composed of upturned Dakota sandstone. Outcrops of the Morrison and the Fountain formations can also be seen. Along the drive is the "Dinosasur trackway," a fenced-off area along the road adjacent to some exposed strata, which showcases the fossilized footprints of ankylosaurs walking towards the west.
The untamed jungle terrain was extremely steep, cut by razor-sharp hogback ridges and required the men to cross a mountain divide. The Australians didn't think it was practical for men to cross on foot. Boice nonetheless reported back that the route was feasible, and the 2nd Battalion, 126th Infantry Regiment was committed to the trail.
The lighthouse served as both the home and workplace of eleven successive keepers and their families. The first floor was divided into a living room and kitchen and the second floor into four bedrooms. Coal stoves provided heat, while large pumps retrieved water from the lake. The keepers used the nearby island to the north, Hogback Island, as farmland.
To the north, a series of ridges separate Rapid Creek from Box Elder Creek. Both older and new residential areas and commercial areas have developed here, along I-90. To the south, the terrain rises more steeply to the southern widening of the Dakota Hogback into a plateau dividing the Rapid Creek drainage from Spring Creek.
Jeremy's Run is a stream in Page County, Virginia. Jeremy's Run originates from rainwater flowing down the west slope of Elkwallow Gap in the Blue Ridge Mountains. Elkwallow Gap is a topographical saddle that divides Neighbor Mountain and Hogback Mountain, situated in Shenandoah National Park. Jeremy's Run flows southwest from the gap, to the Great Appalachian Valley.
The remaining stones are a sarcophagus, five hogback stones and thirty-one recumbent gravestones. Each stone weighs half a ton. and is carved with elaborate designs of carved crosses and cross shafts. The Govan sarcophagus The centrepiece of the collection is the sarcophagus, which is thought to commemorate St. Constantine, the son of Pictish king Kenneth MacAlpin.
The Spartan TV station was originally approved to broadcast from Hogback Mountain, closer to Spartanburg, but sought to move to Paris Mountain, which was then home of WFBC-TV and WGVL and closer to Greenville. For Spartan, this was a necessary condition of obtaining the CBS television affiliation for channel 7; CBS had refused to grant it to a station on Hogback, which it reckoned too close to WBTV in Charlotte, North Carolina. By March 1954, WGVL had already lost $75,000; at that time, its petition to deny the Spartan move to Paris Mountain was denied by the Federal Communications Commission, as had been petitions from WAIM-TV (channel 40) in Anderson and the Sterling Telecasting Company of Spartanburg, which held the construction permit for WSCV (channel 17) in that city.
King Pin () is a nunatak, high, rising above the Wilson Piedmont Glacier, Antarctica, about midway between Mount Doorly and Hogback Hill. It was named by the Victoria University of Wellington Antarctic Expedition, 1958–59, after the American helicopter King Pin which flew the party into this area, and which rendered a similar service in two other years to New Zealand parties.
Colwell Cut Viaduct, also known as Hogback Hill Bridge, is a historic concrete arch bridge located at Mahoning Township in Armstrong County, Pennsylvania. It was built in 1922, and is a three-span bridge, with a main span. It crosses the Pittsburg and Shawmut Railroad. Note: This includes It was listed on the National Register of Historic Places in 1988.
California Department of Conservation, Division of Mines and Geology. Dibblee Foundation Map DF#06. Because the sandstone beds are resistant to erosion, wherever they dip steeply, they form distinctive hogback ridges and dip-slopes, a topography particularly characteristic of the ridge north of Goleta, where the Coldwater accounts for almost all of the terrain above approximately 1,000 feet.Thomas M. Dibblee, 1987.
The Hogback Covered Bridge is a historic covered bridge near Winterset, Iowa. Named after a nearby limestone ridge, it was built in 1884 by Harvey P. Jones and George K. Foster over the North River on Douglas Township Road. The bridge was designed with a Town lattice truss system. It was built with steel pylons to support the main span.
The place demonstrates rare, uncommon or endangered aspects of Queensland's cultural heritage. It is one of the few extant road-rail bridges in Queensland. The place is important in demonstrating a high degree of creative or technical achievement at a particular period. It is the oldest extant of its type in Queensland with the longest hogback span of its type in Queensland.
Gosforth contains a unique collection of Norse artefacts in and around St. Mary's Church. This includes the Gosforth cross, which is the tallest and oldest Viking cross in England. Another high cross was cut down in 1789 to make a sundial base, though the "fishing stone" panel from this survives in the church. There are also two large "hogback" tombs in the church.
The blocks of the slump obstructed wagon traffic west from Fort Hays, which found routes over the Hog Back further south. The railroad, however, was able to cut a roadbed through the slumping. Unfortunately, the slump was not stable and the railroad repeatedly repaired the shifting roadbed over the decades. By the early 1900s, railroad surveyors considered tunneling through the Hogback.
Bellvue is an unincorporated community and U.S. Post Office in Larimer County, Colorado. It is a small agricultural community located in Pleasant Valley, a narrow valley just northwest of Fort Collins near the mouth of the Poudre Canyon between the Dakota Hogback ridge and the foothills of the Rocky Mountains. The ZIP Code of the Bellvue Post Office is 80512.
The is a nation in the New World unaffiliated with the World Government. It has its own warriors, the samurai, who are swordsmen so strong that not even the Navy goes near them. It was first mentioned by Hogback, as Ryuma was from there. In Punk Hazard, the Straw Hat Pirates met two residents of Wano, and his "son" , who temporarily accompanied them on their journey.
Spring Brook begins near Interstate 380 in Covington Township, Lackawanna County. It flows south for a short distance before meandering west for a few miles, crossing Interstate 380 and entering Spring Brook Township. The stream then turns south for several tenths of a mile before turning northwest for several tenths of a mile. It turns southwest before turning north-northwest and flowing around The Hogback.
Roxborough Park is located in northwestern Douglas County at (39.459235, -105.078524). It sits at the foot of the Front Range of the Rocky Mountains. The Dakota Hogback, a prominent sandstone ridge, runs north-south through the community. The CDP is bordered to the west by Pike National Forest, and Roxborough State Park, known for its dramatic sandstone formations, is on the southern edge of the community.
Almost immediately after Congressman Candler offered his pension bill, north Georgia rebels burst into angry protest, calling the soldiers "first Georgia hogback Yankey fellers." In his third term as U.S. Representative, he was the chairman of the Committee on Education. Candler declined to run again in the 1890 election. Candler served as Secretary of State of Georgia from 1894 to 1898 before resigning to pursue the Governorship.
Pignut Mountain is entirely undeveloped. There are no trails or roads leading up the mountain. The summit can be reached by bushwhacking from the Hull School Trail, accessible from Skyline Drive. The closest scenic viewpoints along Skyline Drive from which to view Pignut Mountain are Thornton Hollow Overlook, situated on nearby Neighbor Mountain, Little Devils Stairs Overlook on Hogback Mountain and Rattlesnake Point Overlook on Sugarloaf.
Roxborough State Park is a designated Colorado Natural Area and National Natural Landmark for its 300-million-year-old red sandstone Fountain Formations that tilt at a 60 degree angle. The park includes great examples of exposed Precambrian to Late Mesozoic hogback, monolithic and spire formations from the Permian, Pennsylvanian and Cretaceous age. Carpenter Peak's exposed monzonite is from the Precambrian era.Roxborough State Park: Geology.
The rocks on the west side of Dinosaur Ridge are part of the widespread Morrison Formation of Jurassic age. It is in these rocks, where Arthur Lakes discovered the dinosaur bones in 1877. Fifteen quarries were opened along the Dakota hogback in the Morrison area in search of these fossils. The rocks on the east side of Dinosaur Ridge are part of the Cretaceous Dakota Formation.
The British Museum affirmed the importance of the collection when they took one of the hogback stones to London as part of the exhibition Vikings: Life and Legend (March 2014 to June 2014). In August 2017, the Govan Stones were voted Scotland's best 'hidden gem' in a nationwide competition, receiving more than two thousand votes in the nationwide poll. They have been described as of international significance.
These settlers soon became known as "Free-Staters". Even before the bill passed, some people already had this idea. In early May 1854, four men—Thomas W. and Oliver P. Barber, Samuel Walker, and Thomas M. Pearson—toured the new territory with the intention of finding a good place to settle. Their travels included what would become Lawrence, passing up on the spur of Hogback Ridge.
It provides at least secondary coverage of 94 counties in four states (North Carolina, South Carolina, Georgia and Tennessee). Under the right conditions, it can be heard as far east as Charlotte and as far west as the north Georgia mountains. WSPA is owned by Philadelphia based Entercom Communications. The transmitter tower (which is visible as far as 35 miles away) is located atop Hogback Mountain, near Landrum.
The Colchester Reef Light in Vermont was a lighthouse off Colchester Point (northwest of Burlington, Vermont) in Lake Champlain. It was moved to the Shelburne Museum in Shelburne, Vermont, in 1956. In 1869 the United States Lighthouse Service commissioned the building of the Colchester Reef Lighthouse on Lake Champlain to protect ships from the "Middle Bunch Reef", comprising the Colchester Reef, the Colchester Shoals, and the Hogback Reef.Shelburne Museum. 1993.
Luther is located northeast of Oklahoma City on Oklahoma State Highway 66, formerly U.S. 66. Like many towns between Oklahoma City and Tulsa, Luther was bypassed by opening of the Turner Turnpike in 1953. After decades of planning, a new interchange 11 miles (18 km) east of I-35 was opened at Hogback Road south of Luther in 2011, granting more commuter access between Luther and Oklahoma City.
The Giant's Grave in 1835. The main church is St Andrew's built in 1720–1722 in an imposing Grecian style, abutting a 13th-century tower. The churchyard has ancient crosses and hogback tombstones known as the "Giant's Grave" (early 10th century) and "Giant's Thumb" – remains of a Norse cross from about 920. The ruins of Penrith Castle (14th–16th centuries) can be seen from the adjacent railway station.
Allamakee Trailed vessel from the O'Regan Site Allamakee Trailed vessels from the Hogback Site Archaeologists often find pottery to be a very useful tool in analyzing a Prehistoric culture. It is usually very plentiful at a site and the details of manufacture and decoration are very sensitive indicators of time, space and culture. Pottery was found at all 7 sites. The analysis was based on 17 complete vessels and 2,072 sherds.
The underlying rocks are dipping slightly to the east. The eastern (and newer) side of the valley is underlain primarily by Pierre Shale laid down during Cretaceous time. The western (and older) side of the valley, on the west side of Red Hill, is underlain primarily by Permian and Pennsylvanian rocks. Red Hill runs through the center of the valley as a hogback ridge of tilted Cretaceous and Jurassic sedimentary rocks.
The upright sides of the house are covered with interlacing flat bands on one side, and the walls are strengthened with pilasters highly ornamented. A broad one in the middle and a narrower one at each end (one end having been broken away). The other side is much damaged, but shows evidence of knot work of double strands. The Hogback is now in the vestry, close to the Font.
The San Juan Basin is an asymmetrical syncline with three components: the Central Basin Platform, the Four Corners Platform, and the Chaco Slope (a.k.a. the Chaco Homocline). The basin is bound on the northwest by the Hogback Monocline (separating the Central Basin and Four Corners platforms), on the northeast by the Archuleta Anticlinorium, on the east by the Nacimiento Uplift, and on the south by the Zuni Uplift.
In a niche at the east end of the aisle are two carved Viking hogback stones. These are very rare pre-Norman tomb markers that were found under the foundations of a 12th- century wall of the church during restoration in 1896-97. The early 11th century is the latest possible date.C A Parker, The Gosforth District, 1904 The hogbacks are each in the shape of a house.
Sallee and Rumsey came through the hogback to the ridge crest above what became known as Rescue Gulch. Dropping down off the ridge, they managed to find a rock slide with little to no vegetation. They waited there for the fire to overtake them, moving from the bottom of the slide to the top as the fire moved past. Hellman was caught by the fire on the top of the ridge and was badly burned.
In Lancashire, the Heysham hogback may depict Sigurd stabbing Fafnir through the belly as well as his horse Grani. It is one of the few monuments on the British Isles that does not appear to have been influenced by Christianity. The nearby Halton cross appears to depict Regin forging Sigurd's sword and Sigurd roasting Fafnir's heart, sucking his thumb. The iconography of these depictions resembles that found on the Isle of Man.
KTVH-DT, virtual and VHF digital channel 12, is an NBC affiliated television station licensed to Helena, Montana, United States. Owned by the E. W. Scripps Company, it is a sister station to low-powered CBS affiliate KXLH-LD (channel 9). The two stations share studios on West Lyndale Avenue in Helena; KTVH's transmitter is located on Hogback Mountain. KTVH is simulcast on KTGF-LD channel 50 (Charter Spectrum cable 6) in Great Falls.
Meteorite Mountain is a prominent glaciated mountain summit located in the Chugach Mountains, in the U.S. state of Alaska. It is situated southeast of Valdez, south of Hogback Ridge, and southeast of Mount Francis. In January 1927, a meteorite hit this mountain, which is how the mountain got its name.The Valdez Miner, July 9, 1927 The mountain's name was in local use when it was first published in 1953 by U.S. Geological Survey.
The Lower Coulee, also created its own path across the plains. Evidence of this is found in the tilted flows visible at Hogback islands in Lake Lenore and tilted flows along Washington 17 from Dry Falls to Park Lake. Numerous canyons acted as a distribution system for the volume of water flowing out of the upper coulee. The distribution begins in the uncanyoned basin below Dry Falls and expanded to over before reaching Quincy Basin.
East of there, SR 521 passes through woodlands as it crosses over Alum Creek and passes its intersection with Hogback Road. As it re-enters primarily open farmland, SR 521 passes Kilbourne Road, then follows an S-curve to the southeast. Resuming an easterly trek, after passing the unusually-named 3 Bs & K Road, SR 521 crosses into Kingston Township. Next, the state highway crosses Galena Road, then passes over Interstate 71 without an interchange.
Dinosaur Ridge is a segment of the Dakota Hogback in the Morrison Fossil Area National Natural Landmark located in Jefferson County, Colorado, near the town of Morrison and just west of Denver. The Dinosaur Ridge area is one of the world's most famous dinosaur fossil localities. In 1877, fossil excavation began at Dinosaur Ridge under the direction of paleontologist Othniel Charles Marsh.McCarren, Mark J. The Scientific Contributions of Othniel Charles Marsh, pp.
Monoclines form as a result of uplift bending the rock units. Eroded monoclines leave steeply tilted resistant rock called a hogback and the less steep version is a cuesta. Cliffs of Navajo Sandstone in Zion National Park Great tension developed in the crust, probably related to changing plate motions far to the west. As the crust stretched, the Basin and Range province broke up into a multitude of down-dropped valleys and elongate mountains.
Captain Hildreth Frost led a small group of National Guard troops on 28 April in the northernmost battle at a nine in Louisville. The same day, a National Guard medic was killed and several wounded in a firefight for the hogback near Walsenburg. The fighting ceased on 29 April after President Woodrow Wilson ordered the federal-level Army to disarm the strikers and turn-back the National Guard. The strike concluded without much further violence in December 1914.
Following this further west, one can see the biggest mountain in the immediate foothills west of the Manor House, Tincup Mountain (Beacon Hill can also be seen- the shoulder on the south side of Tincup). The hogback (the ridge/rift running along the east side of the valley, opposite of the Foothills, that helps form the valley) is an interesting geologic phenomenon as well, formed from sedimentary layers being pushed upwards around 70 million years ago.
These landmarks represent a distinctive style of construction and are enduring monuments to George Morrison's contributions to Jefferson County's history. Stone for these structures was quarried in his "red sandstone quarry" at the end of the Dakota Hogback near Morrison. Building stone was also shipped to Denver, where it now comprises parts of the Brown Palace Hotel, Union Station, and "many of Denver's early day mansions". Mount Morrison behind Red Rocks Park is also named after George Morrison.
The door-surround is enriched with two bands of pellets, and the monolithic arch has a well-preserved representation of the Crucifixion. The slightly splayed sides of the doorway (also monolithic) have relief sculptures of ecclesiastics, one of them holding a crosier, the other a Tau-shaped staff. Two monuments preserved within the cathedral, the so-called 'Brechin hogback', and a cross-slab, 'St. Mary's Stone' are further rare and important examples of Scottish 11th century stone sculpture.
The Dickabram Bridge over the Mary River is long and stands above the Mary River. All spans are metal trusses except for the approach spans which are tied timber girders. The two river piers are cast iron cylinders; the remaining piers and road deck are timber. It comprises two parallel chord lattice girder spans either side of a hogback lattice girder span, having steel cross girders, supported on two cylinder piers and two double timber piers.
New Castle is located at (39.572304, -107.534941), on the north side of the Colorado River, just east of where the river cuts through the Grand Hogback. Interstate 70 passes through the town following the river, with access from Exit 105. I-70 leads east to Glenwood Springs, the county seat, east to Denver, and west to Grand Junction. U.S. Route 6 is Main Street in New Castle and forms a parallel route to I-70 for local traffic.
Subsequent features include Musselman Arch, Airport Tower butte, Monster Tower, and Washer Woman Arch, all visible from the road. A steep spur road leads down to the Colorado River through Lathrop Canyon. Back on the White Rim Road, one passes Buck Canyon, Gooseberry Canyon and Monument Basin with its rock pinnacles, followed by the White Crack campground spur road. The next challenge occurs at the steep Murphy Hogback which marks the approximate halfway point on the road.
The road is rated moderately difficult for high-clearance, four-wheel drive vehicles in good weather conditions. The most difficult sections are the switchbacks of the Shafer Trail and Mineral Bottom Road, the Lathrop Canyon Road (an optional spur road), Murphy Hogback, and Hardscrabble Hill. Portions of the road near the Green River may be flooded during high water events. Horses and pack animals such as burros and mules are allowed on all backcountry roads with a permit.
He brought his wife, Emeline, and his family west from Anamosa, Iowa. Over the years, he acquired of land. The family used homesteading of for each qualified members of the family, they purchased military patents, State land grant college lands, Union pacific lands, and from other homesteaders. The ranch ran from the hogback on the west to the South Platte River on the east, from Bear Creek on the south to Table Mountain near Golden on the north.
The outermost feature of the dome stands out as a hogback ridge. The ridge is made out of the Lakota Formation and the Fallriver sandstone, which are collectively called the Inyan Kara Group. Above this, the layers of rocks are less distinct and are all mainly grey shale with three exceptions: the Newcastle sandstone; the Greenhorn limestone, which contains many shark teeth fossils; and the Niobrara Formation, which is composed mainly of chalk. These outer ridges are called cuestas.
Graham-Campbell and Batey (1998) pp. 96–98 Five Hogback monuments found in Govan hint at Scandinavian enclaves inland.Graham-Campbell and Batey (1998) pp. 100–01 The Isle of Man (which was absorbed into Scotland from 1266 until the 14th century) was dominated by the Norse-Gaels from an early date and from 1079 onwards by the Crovan dynasty as attested by the Chronicles of Mann and evidenced by the numerous Manx Runestones and Norse place names.
Structurally, the Marlboro Mountains constitute a geologic formation known as a dip slope. The sedimentary layers comprising the bulk of the mountains dip towards the west, with a hard cap rock layer at the surface. The ridgeline of the mountains forms the edge of the cap rock layer, which is being eroded relatively slowly, protecting underlying geologic layers from being weathered. This setup leads to the hogback appearance of the mountains: gently sloping westward flanks and steeply graded eastern flanks.
View from Rhüden to the Heber Glasworks in the Westerhof Abbey Forest near the Heber The Kopfbuche beech near Gremsheim The ridge measures roughly 10 km long by around 1 to 2 km wide and is covered by beech and spruce forests. The highest elevation of the Heber is the Mechtshäuser Berg in the borough of Seesen at . Geologically it is a hogback formed predominantly from limestone. Southwest of the Heber is the Heber-Börde, a basin-like countryside with fertile loess soils.
Mount Francis is a glaciated mountain summit located in the Chugach Mountains, in the U.S. state of Alaska. This landform is situated southeast of Valdez, southwest of Hogback Ridge, and northwest of Meteorite Mountain. This feature was named in 1898 by Captain William R. Abercrombie who led an 1898 expedition seeking a route from coastal Alaska to the Klondike. Precipitation runoff and meltwater from the mountain's glaciers drains into tributaries of the Lowe River, which in turn empties to Prince William Sound.
Dickabram Bridge was listed on the Queensland Heritage Register on 21 October 1992 having satisfied the following criteria. The place is important in demonstrating the evolution or pattern of Queensland's history. The bridge is a late 19th-century and essentially unmodified high level road-rail bridge with half-through double by 2 lattice girder approach spans and hogback through double x 2 lattice girder main spans. It was constructed on the site of several low-level bridges that had been destroyed by floods.
KUHM-TV, virtual channel 10 (UHF digital channel 29), is a Public Broadcasting Service (PBS) member television station licensed to Helena, Montana, United States. Owned by Montana State University (MSU), the station is operated as part of the Montana PBS state network (a joint venture with the University of Montana (UM)). KUHM-TV's transmitter is located on Hogback Mountain; master control and internal operations are based at the network's headquarters in the Visual Communications Building on the MSU campus in Bozeman.
Hogback Mountain is part of Catoctin Mountain, located southwest of Leesburg in Loudoun County, Virginia. The mountain ridge rises immediately to the west of U.S. Route 15, just south of Sycolin Creek and extends south to the banks of Goose Creek. It is so named for its appearance when approaching it from the north of resembling a pig on its back. The ridge is mislabeled on older USGS topographic maps as being located to the north, between Sycolin Creek and Leesburg.
The stone demonstrates stylistic affinities with early hogback stones from the Glasgow area. The ridge of the stone is carved with an elongated beast with its head at the higher end of the monument, the beast has the tail of a fish at the tapering end if the stone. The creature's head is similar to the heads of animals on Meigle 1 and Meigle 5. Meigle 27 depicting a figure seated in a chair with his servant sitting on the floor behind.
The Transylvania Times is an American, English lanuage bi-weekly newspaper in Transylvania County, North Carolina, in the United States, and its surrounding area. The paper was founded in 1887, and is family-owned and operated. It provides news coverage for Brevard, Pisgah Forest, Rosman and Lake Toxaway, as well as the townships of Cathey's Creek, Dunn's Rock, Eastatoe, Gloucester, Hogback and Little River. The paper has a circulation of approximately 7,700 and averages about 15,000 readers per print edition.
Shaped like a hogback, it came to be known as Hog Island, or sometimes as Far Rockaway Beach Island. The island attracted developers of various seafront beach resort businesses, including leisure pavilions, bathing facilities, saloons, restaurants. It was a favorite getaway of Tammany Hall politicians, and many "backroom deals" were actually concluded in the open air here. A winter storm in early 1893 severely damaged the island. In late August 1893, several hurricanes were simultaneously active in the Atlantic Ocean.
The current church in Narborough dates from the 13th century, although it is highly probable an even earlier church dating back to the 10th century or before stood on or near the site. A Saxon hogback tombstone was found near the church and is on display at the Jewry Wall Museum in Leicester. The church was largely rebuilt in 1856–1883. There are two aisles, nave, chancel and north vestry with a west tower containing a ring of six bells.
Goshen and Little North Mountain Wildlife Management Area is a protected area located in Rockbridge and Augusta counties, Virginia. At , it is the largest Wildlife Management Area managed by the Virginia Department of Game and Inland Fisheries. The area comprises two parcels of land bisected by the Maury River; the lowest terrain is above sea level, while the highest is . Three major mountains (Bratton, Forge, and Hogback) are found within the heavily forested area, in addition to a lesser amount of native herbaceous habitat.
To the north of the ridge lies the London Clay, and to the south the clays of the Wealden Group. The chalk is more resistant to weathering than the flanking clays, leading to the ridge's prominence over the surrounding terrain. The Hog's Back gives its name to the geomorphological landform known as a Hogback, which is a long narrow ridge or series of hills with a narrow crest and steep slopes of nearly equal inclination on both flanks.Huggett, JR (2011) Fundamentals of Geomorphology, 3rd ed.
Quinebaug Woods is a open space preserve located in Holland, Massachusetts. The property, acquired in 2001 by the land conservation non-profit organization The Trustees of Reservations, is named for the Quinebaug River, which runs through the reservation. The reservation is located off Dug Hill Road in northeast Holland and offers of hiking trails, woodlands, river frontage, a scenic vista, and the remains of a 1930s cabin atop the hogback Blake Hill. The reservation is open to hiking, picnicking, horseback riding, fishing, and cross country skiing.
Elliott Knob is one of the highest mountains in the northern portions of the U.S. state of Virginia. At , the peak is located on the ridge known as Great North Mountain. A subpeak known simply as "Hogback" () is located to the southwest. A small, naturally growing stand of red spruce trees is on the summit, and the upper slopes also have yellow birch and sugar maple, indicating that the altitude is just high enough to support tree species normally found hundreds of miles to the north.
Wiley Schoolhouse (built 1874) is a fully restored historic one-room school for the former District #11 located at the intersection of Wiley (CR 374), Hogback and Olmstead roads in the southwest part of town.Wayne County Office of the County Historian - Savannah, New York, Retrieved Feb. 3, 2015 The Crusoe House (built 1824), located on N.Y. Route 89 near Crusoe Lake, is currently the oldest building in the Town of Savannah. Originally a hotel and tavern, the first ever town meeting was held there in April 1825.
On 28–29 April, the National Guard fought strikers in the Battle of Walsenburg for control of the town and the hogback which overlooked it. Two strikers were killed on the 28th, including one by friendly fire. Colonel Verdeckerg, who placed in command of the Guard at Ludlow following the massacre, was ordered by Chase to take 60 men to Walsenburg to retake the town on the morning of the 29th. Verdeckberg was ordered to hold the town until federal troops arrived then retire back.
Situated between the two sets of spans was a horizontally turning swing bridge of of asymmetric hogback plate girder design with a clear space when open of . The bridge opened in 1872. In 1873 the Manchester, Sheffield and Lincolnshire Railway was enabled by an act () to build a short line connecting from their line (Great Grimsby and Sheffield Junction Railway) near Great Coates to the Old Dock. Logan and Hemingway obtained the contract to construct the line with a bid of £3,984, and construction began in November 1878.
Historically in the County of Dunbarton, its original name is Clachan dhu, or 'dark village'. Ben Lomond, the most southerly Munro, dominates the view north over the loch, and the Luss Hills rise to the west of the village. Saint Kessog brought Christianity to Luss at some uncertain date in the 'Dark Ages'. A number of early medieval and medieval monuments survive in the present churchyard, including simple cross- slabs which may date to as early as the 7th century AD, and a hogback grave- cover of the 11th century.
Hjorth Hill () is a rounded, ice-free mountain, high, standing just north of New Harbour and south of Hogback Hill, in Victoria Land, Antarctica. The hill is separated from the MacDonald Hills by Quinn Gully. It was charted by the British Antarctic Expedition, 1910–13, led by Robert Falcon Scott, and was named for the maker of the primus lamps used by the expedition. The name is spelled "Hjort's Hill" in the popular narrative of Scott's expedition, but "Hjorth's Hill" is used on the map accompanying the narrative.
In 2000, the Roaring Fork Transportation Authority was created by seven members in the Roaring Fork Valley, creating the state's first Rural Transportation Agency and taking over the responsibilities of the Roaring Fork Transit Agency. As a result of the vote, RFRHA merged with the RFTA in 2001. In 2004 the Town of New Castle voted to become the newest member of RFTA. Rifle and Silt, west of New Castle along the I-70/US 6 corridor, are not members but still receive RFTA service on the Grand Hogback route.
For over ten years Professor Haller and his family- his wife, Malleville and their three children, Bill Jr., Ben and Maria- rented a cottage on Holland Pond where they spent their summers. Then, in 1931, Haller purchased nearly one hundred acres of woodland on the west bank of the Quinebaug River. The land included a hill just north of the Hamilton Reservoir dam that was referred to locally as a “hogback”- an exposed rocky ridge. An old logging road ran to the top of the hill and, here, the Hallers built a cottage.
On 20 November 1942, after almost 42 days trekking across exceedingly difficult terrain, including hogback ridges, jungle, and mountainous high-altitude passes, E Company of the 128th was the first to reach Soputa near the front. The remainder of the Battalion trickled in over the next few days. As a result of the extremely difficult march and the decimated ranks of the unit, the battalion earned the nickname of The Ghost Battalion. By the time the troops reached Soputa, they were in such bad shape they weren't fit for combat.
The earliest English church monuments were simple stone coffin-shaped grave coverings incised with a cross or similar design; the hogback form is one of the earliest types. The first attempts at commemorative portraiture emerged in the 13th century, executed in low relief, horizontal but as in life. Gradually these became full high-relief effigies, usually recumbent, as in death, and, by the 14th century, with hands together in prayer. In general, such monumental effigies were carved in stone, marble or wood, or cast in bronze or brass.
There are upper and lower churchyards, where men and women respectively were buried; both have a large number of fairly worn grave slabs, one or two of which have traces of decoration. In the lower churchyard there are the remains of another building thought to have been of a small chapel. In the upper churchyard is a hogback tombstone, often wrongly said to mark the tomb of St Blane, and which dates to the 900s or 1000s. It shows that the Norsemen who settled here, after the monastery was abandoned, eventually became Christians themselves.
View near Horsetooth Horsetooth Reservoir (often known locally as Horsetooth) is a large reservoir in southern Larimer County, Colorado, just west of the city of Fort Collins, Colorado. The reservoir sits in the foothills above the town on the western side of the Dakota Hogback, which contains the reservoir along its eastern side. The reservoir runs north-south for approximately 6.5 miles (10 km) and is approximately one-half mile (1 km) wide. It was constructed in 1949 by the Bureau of Reclamation as part of its federal Colorado-Big Thompson Project or "C-BT".
Goole railway swing bridge, over the River Ouse The Skelton Viaduct, also known as the Hook bridge or Goole railway swing bridge, is a large viaducted hogback plate girder bridge with swing span over the River Ouse, Yorkshire near Goole. The bridge was designed by Thomas Elliot Harrison for the Hull and Doncaster Branch of the North Eastern Railway and opened in 1869. In the latter part of the 20th century, the bridge became known for the frequent incidents involving ship collisions with the superstructure. As of 2020, it is still in use.
Although called by some 'pagan' or 'Viking', it may be that some, if not most, of the crosses and hogback sculpture (to be found almost wholly in south Cumbria, away from the Strathclyde area), such as the Gosforth Cross and the Penrith 'Giant's Grave', reflect secular or early Christian concerns, rather than pagan ones.Bailey (1985), p. 61. Due to the lack of documentary corroboration or of inscriptions on the sculptures themselves, we are thrown back on comparative analyses of the ornamentation and other stylistic indicators.Bailey (1980), ch. 3.
Plush School in 2015 By highway, Plush is about northeast of Lakeview and north of Adel in the Warner Valley of south-central Oregon.Google Maps Plush–Adel Road runs north–south along the valley floor, while Plush Cutoff links Plush to Oregon Route 140 west of Adel. Hogback Road runs north from Plush, while Hart Mountain Road, which terminates in Plush, runs east and northeast to the Warner Wetlands Area of Critical Environmental Concern and the Hart Mountain National Antelope Refuge. Hart Lake, at the base of Hart Mountain, is about east of the community.
Located near the town of Morrison, off U.S. Route 285, the site is located in the southern Rocky Mountains foothills, at about elevation, where uplifted Dakota Sandstone formed a steep hogback. The rockshelter is sheltered by distinctive 60 foot "red rock" formation, caused by an uplift of Fountain Formation rock. The Morrison area is between the locations of two important early people: Desert societies of the Great Basin west of the Rocky Mountains and those of the Great Plains, which lies to the east of the Rocky Mountain foothills.Irwin, Henry J., and Cynthia C. Irwin.
Mount Oread is a hill in Lawrence, Kansas upon which the University of Kansas, and parts of the city of Lawrence, Kansas is located. It sits on the water divide between the Kansas River and the Wakarusa River rivers. It was named after the long defunct Oread Institute in Worcester, Massachusetts, where many of the settlers of Lawrence moved from prior to the American Civil War. The hill was originally called Hogback Ridge by many Lawrence residents until the Oread name was adopted in 1864, two years after the university was founded.
East Peak is a glaciated mountain summit located in the Chugach Mountains, in the U.S. state of Alaska. The peak is situated east of Valdez, northeast of Mount Francis, and immediately north of Hogback Ridge. Although modest in elevation, relief is significant since the western aspect of the mountain rises up from tidewater of Prince William Sound in approximately six miles. The mountain received its descriptive name in 1898 from Captain William R. Abercrombie, who led an 1898 expedition seeking a route from coastal Alaska to the Klondike.
During this period, the Oregon Trail ran parallel to the Kansas River, roughly through the area where Lawrence is now. A hill in the area, then known as Hogback Ridge and now known as Mount Oread, which sits on the water divide separating the Kansas and Wakarusa River, was used as a landmark and outlook by those on the trail.Andreas (1883), pp. 30809. While the territory was technically closed to settlement until 1854, there were a few "squatter settlements" in the area, especially just north of the Kansas River.Nelson (1995).
As the rest of the crew came up, Dodge tried to direct them through the fire he had set and into the center burnt out area. Dodge later stated that someone, possibly squad leader William Hellman, said "To hell with that, I'm getting out of here". The rest of the team raced past Dodge up the slope toward the hogback of Mann Gulch ridge, hoping they had enough time to get through the rock ridge line to safer ground on the other side. None of the men trying to outrun the fire entered the area Dodge had burned.
Private First Class Kerstetter official Medal of Honor citation reads: > He was with his unit in a dawn attack against hill positions approachable > only along a narrow ridge paralleled on each side by steep cliffs which were > heavily defended by enemy mortars, machineguns, and rifles in well- > camouflaged spider holes and tunnels leading to caves. When the leading > element was halted by intense fire that inflicted 5 casualties, Pfc. > Kerstetter passed through the American line with his squad. Placing himself > well in advance of his men, he grimly worked his way up the narrow steep > hogback, meeting the brunt of enemy action.
Tremendous thrusts piled sheets of crust on top of each other, building the extraordinarily broad, high Rocky Mountain range. Tilted slabs of sedimentary rock in Colorado The current southern Rockies were forced upwards through the layers of Pennsylvanian and Permian sedimentary remnants of the Ancestral Rocky Mountains. Such sedimentary remnants were often tilted at steep angles along the flanks of the modern range; they are now visible in many places throughout the Rockies, and are prominently shown along the Dakota Hogback, an early Cretaceous sandstone formation that runs along the eastern flank of the modern Rockies.
A new double track swing bridge had also been constructed over the Hull, , slightly to the north of the original single track bridge. The bridge was designed by NER staff J. Triffit under W.J. Cudworth, and erected by R Woods (Westminster) with steelwork from John Butler & Co. (Stanningley): a 75°33' skew, made of plate girders to a maximum depth hogback design, long total. The bridge turning mechanism was electrically powered, using Siemens Bros. equipment, and controlled by a cabin above the bridge; the designer was Wilson Worsdell, also of the NER, and the contractors Cowans and Sheldon.
If the elevated comb is of a rounded dome shape, it is often called a hogback comb. A cheekpiece (C) is a raised section on the side of the stock, which provides a more comformed support for the shooter's cheek. There is some confusion between these terms, as the features are often combined, with the raised rollover cheekpiece (D) extending to the top of the stock to form essentially a high Monte Carlo comb. Some modern buttstocks have a movable comb piece called a cheek rest or cheek rise, which offers adjustable comb height that tailors to the shooter's ergonomic preference.
Sunset Island is a three-acre island on Lake Champlain, located just west of the Greater Mallets Bay, Colchester, Vermont, United States. It is currently privately held, with Patricia McDonald as the majority owner. Originally named Hogback Island, the property was used by the caretaker of the Colchester Reef lighthouse for farming from 1871 until the lighthouse was decommissioned in 1933. In 1956, after the lighthouse had been relocated to the Shelburne Museum, Sunset Island went up for auction and was purchased by John McDonald and 3 other sportsmen to be used predominately for duck hunting.
Originally they had ling thatched roofs, but they were mostly re-roofed in the 19th century with grey slate or red pantiles. All Saints' Church has in its fabric an assemblage of dozens of fragments of pre-Norman crosses and hogback fragments scattered all over the building, inside and out. It appears that several - perhaps the numbers even reach double figures - significant crosses were broken up in order to provide building stone for the twelfth-century workers who built the church. Catherine Parr was resident in the manor of Sinnington, as Lady Latimer, between 1534 and 1543.
Around this time, it increased the stock issue to $5,000,000 and issued an additional $5,000,000 in fifty-year bonds. The Clearfield Bituminous Coal Company signed a contract to ship exclusively over the new railroad, and George Magee was appointed general contractor for construction. The new line was built to high standards in anticipation of heavy coal traffic. It eschewed severe grades, at the cost of extensive curvature and bridges as it followed Beech Creek, and the Hogback tunnel, which cut across a loop of the creek, about halfway up the climb out of the watershed at Hurxthal's Summit.
The station in its initial years on air operated under special temporary authority at just 1,000 watts. It would not be until December 1957 that channel 62 broadcast at its intended effective radiated power of 24,000 watts. In 1964, Spartanburg CBS affiliate WSPA-TV improved its service to Asheville by building a translator on channel 72 at White Fawn Reservoir, which provided a stronger signal and reached homes shaded from its main transmitter at Hogback Mountain. During the application process, it was noted that WISE-TV aired little more than NBC network shows and "extremely limited" live programming.
To begin this hike you must proceed up the Tower Road and pass by the gated road which leads to Herman Point and the transmitter towers on its summit. Just behind the fenced in towers, you can see the trail which proceeds down the steep face of the mountain into the Rhodes Run drainage. From here the trail follows Ciana Run before crossing Hogback ridge, then beginning its steep ascent up Forks Ridge and the Allegheny Front beyond. Once on top of the Allegheny Plateau it winds its way through high elevation forests and mountain bogs.
Staff Sergeant Laws' official Medal of Honor citation reads: > He led the assault squad when Company G attacked enemy hill positions. The > enemy force, estimated to be a reinforced infantry company, was well > supplied with machineguns, ammunition, grenades, and blocks of TNT and could > be attacked only across a narrow ridge 70 yards long. At the end of this > ridge an enemy pillbox and rifle positions were set in rising ground. > Covered by his squad, S/Sgt Laws traversed the hogback through vicious enemy > fire until close to the pillbox, where he hurled grenades at the > fortification.
Soon after the Hogback, the Turks Head butte appears in the middle of an oxbow bend of the Green River. Candlestick Tower and Potato Bottom are next, followed by a round-trip hiking trail to Fort Bottom Ruin and then a steep, rocky section of road at Hardscrabble Hill. Finally, a spur road leads to two rock towers called Moses and Zeus. After crossing sandy dry washes, or arroyos, the White Rim Road ends just outside the national park boundary at the junction with Mineral Bottom Road and its hairpin turns leading one back up to the Island in the Sky.
The White River Plateau is a "broad structural dome" located north of Glenwood Springs, Colorado and north of the Colorado River. Also called the White River Uplift, the mountainous area is shown on maps as being roughly circular in area, occupying parts of the Colorado counties of Garfield and Rio Blanco, with small portions extending into Eagle and Routt counties. The Grand Hogback marks parts of the plateau's southern and western boundaries. The Flat Tops mountain range is part of the White River Plateau, and much of the plateau is located within the White River National Forest.
SH 470 begins in Golden as an extension of Johnson Road at an intersection with US 6 (6th Avenue) near the Jefferson County government office complex and its adjacent light rail station. The interchange also includes direct ramps to westbound US 6, which continues northwest towards central Golden and east to Denver. SH 470 travels south from the intersection on a four-lane freeway and passes over US 40 before reaching an interchange with I-70 near Tin Cup Hogback Park. The freeway expands to six lanes and continues south along the side of Green Mountain on the western outskirts of Lakewood.
It intersects SH 8 at a single-point urban interchange in Morrison near the Bandimere Speedway complex. From Morrison, SH 470 begins a gradual turn to the southeast as it passes between Mount Glennon and Bear Creek Lake Regional Park. It intersects US 285, a minor freeway that travels east through Lakewood, and continues south with four lanes along the edge of a hogback at the edge of the Denver area's suburban sprawl, served by several exits on the freeway. SH 470 turns east in Ken Caryl near Hildebrand Ranch and intersects SH 121 at the western edge of the Chatfield Reservoir.
The central river pier had similar foundations of two 8 ft cast iron piers braced together. The swing span turntable consisted of diameter steel conical roller paths and bearings, supported on a circular deep box girder in eight sections, with a twelve section box girder above, supporting the superstructure. The bridge turned about a central heavy cast pivot, with ties to the upper and lower box girders, and to the bearings. The bridge superstructure was constructed of wrought iron plate girders, with an asymmetric 'hogback' shape; the swing span extremities were from the centre line, with a counterweight; the maximum web depth was .
The Sadliers Crossing Railway Bridge is a rare surviving example of the use of riveted double-intersection through Pratt trusses (Whipple trusses), and is the second longest span of this type in Queensland. This bridge and the former Burdekin River Rail Bridge are the only parallel chord examples of the Whipple design extant in Queensland. A variant of the Whipple truss design, using hogback trusses, is used in the Albert Bridge, Indooroopilly and the Alexandra Railway Bridge, Rockhampton. The cantilevered pedestrian footbridge and access stairs attached to the upstream spans is a rare example of its type and is still in use.
Bicycles and other non-motorized vehicles, normally prohibited on Interstate Highways, are allowed on those stretches of I-70 in the Rockies where no other through route exists. The U.S. Department of Transportation (USDOT) lists the construction of I-70 among the engineering marvels undertaken in the Interstate Highway system, and cites four major accomplishments: the section through the Dakota Hogback, Eisenhower Tunnel, Vail Pass and Glenwood Canyon. The Eisenhower Tunnel, with a maximum elevation of and length of , is the longest mountain tunnel and highest point along the Interstate Highway System. The portion through Glenwood Canyon was completed on October 14, 1992.
This portion features grade-warning signs with unusual messages, such as "Trucks: Don't be fooled," "Truckers, you are not down yet," and "Are your brakes adjusted and cool?" Runaway truck ramps are a prominent feature along this portion of I-70, with a total of seven used along the descent of either side the Continental Divide to stop trucks with failed brakes. Warning sign stating, "Trucks, Don't be Fooled—4 more miles of steep grades and sharp curves." The last geographic feature of the Rocky Mountains traversed before the highway reaches the Great Plains is the Dakota Hogback.
The community is lush area on the south side of the Cache la Poudre River, at the mouth of Rist Canyon, concealed from the open Colorado Piedmont near Fort Collins and LaPorte by the Bellvue Dome, also known as "Goat Hill". The valley formerly stretched southward between the hogback and foothills into the area now inundated by Horsetooth Reservoir. The main agriculture in the valley is cultivation of hay and other crops, as well as cattle and horse ranches. The Colorado Division of Wildlife maintains a large trout hatchery in the valley just north of the Bellvue town site.
Four of the men reached the ridge crest, but only two, Bob Sallee and Walter Rumsey, managed to escape through a crevice or deep fissure in the rock ridge to reach the other side. In the dense smoke of the fire, the two had no way of knowing if the crevice they found actually "went through" to the other side or would be a blind trap. Diettert had been just to the right, slightly upgulch of Sallee and Rumsey, but he did not drop back to the crevice and continued on up the right side of the hogback. He did not find another escape route and was overtaken by the fire.
The Tooth of Time, as well as Baldy Mountain, Betty's Bra, Lover's Leap, Cathedral Rock, Hogback Ridge, and many of the ridges in the northwest of the ranch, is an igneous intrusion of dacite porphyry formed in the Paleogene Period of the Cenozoic Era some 22-40 million years ago. These intrusions were formed when magma from deep within the Earth rose through older rock layers and slowly cooled. Over many thousands of years, the older sedimentary rock eroded and left the harder igneous formation. The sedimentary rock, generally shale, acted as a mold for the intrusive magma, causing it to harden and cool where the sedimentary rock was strongest.
It may have served the monks of the Columban family as an "Iona of the east" from early times. A primitive stone- roofed building survived on the island, preserved and given a vaulted roof by the monks of the later abbey, probably served as a hermit's oratory and cell in the 12th century, if not earlier. Fragments of carved stonework from the Dark Ages testify to an early Christian presence on the island. A hogback stone, preserved in the abbey's visitor centre, can be dated to the late 10th century, making it probably Scotland's earliest type of monument originating among Danish settlers in northern England.
At Woolsey, US 15 meets the northern end of SR 234 (Sudley Road) and reduces to two lanes. North of Bull Run, where the road enters Loudoun County, the highway passes through a pair of roundabouts at Gilberts Corner. US 15 meets US 50 (John Mosby Highway) at the second roundabout. The U.S. Highway runs along the east flank of the Bull Run Mountains as it passes James Monroe's estate of Oak Hill just south of the Little River and Oatlands Plantation in the community of Oatlands at its crossing of Goose Creek. At Virts Corner east of Hogback Mountain, US 15 enters the town of Leesburg as South King Street.
Stout as mapped in 1906 Stout is a former town in southern Larimer County, Colorado in the United States. The town was located in foothills southwest of Fort Collins, just west of the Dakota Hogback. It was established in the 1860s as a camp for workers at the nearby stone quarries in the area. The Union Pacific Railroad invested in quarrying operation in the valley around the town, and at one time Colorado and Southern RailwayUSGS Fort Collins 1906 1:62500 topo built a spur of their rail line from Fort Collins up to the town in order to transport stone for its own use.
The Bungalow type, while not as common as the preceding four, was prevalent between the 1920s and 1930s. Many of the vernacular Gothic Revival and I-House dwellings, which line Locust Street in the Hogback neighborhood south of the mill, date from the late 1860s to 1870s. Farther away from the mill, on a hillside at the east end of the district, stand dozens of Four-Squares, Gable Fronts, and late Gothic Revival types built after the mill expansions of 1898 and 1912. These examples are found along New, Poplar, Walnut and Cherry Streets. Bungalow types from the 1920 to 1930s are scattered throughout the district in wood or brick.
Architecturally, Roaring Spring's neighborhoods display relatively little hierarchy by income or occupation. Admittedly, some areas, like the Hogback just south of the paper mill, were especially known as mill workers' enclaves, but overall the town lacks the strong homogeneity of worker house types and segmentation by occupational class common to coal company towns. D. M. Bare and his cohorts seemed to have envisioned Roaring Spring as a working community of middle- class homeowners plucked from the ranks of shopkeepers, professionals and skilled workers. The relative success of this ideal may be accounted for by the large number of skilled workers required for paper and book-making.
The barrel is polished whereas the receiver has a matte finish; both are blued. The barrelled action sits in a walnut stock in the European-style with checkered grip, schnabel fore-end, and arched (curved) comb sometimes referred to as a Bavarian or "hogback" stock, and is trimmed with European sling swivels and a hard plastic butt plate. The lower drop at the heel and arched comb of the stock are designed to aid shooting with iron sights. The rear tangent sight is graduated in 25 meter increments with calibrated markings from 25 to 200 meters, while the sight leaf is adjustable for windage.
South of Hogback and Leon Creek the range becomes much more rugged as it narrows. Mount Birch 2232 m (7323 ft), just south of Leon Creek, is named after the Lieutenant-Governor who ran the Crown Colony of British Columbia for most of the alcoholic Frederick Seymour's term as governor. Birch has a twin summit on its short, sharp ridge - Mount Duncan 2182 m (7159 ft) and a southern foreshoulder overlooking the confluence of the Yalakom and Bridge Rivers is named Mount Bishop . From Bishop south to the Fraser the boundary of the range is the very lower stretches of the Bridge River, after its confluence with the Yalakom.
The formation is likely an early Cretaceous geologic unit, with its northern exposure running north and south within the Front Range foothills and the Dakota Hogback in northern Colorado and southern Wyoming where it is assigned formation rank within the Dakota Group. In south-central Colorado, the Lytle is a member of the Purgatoire Formation. The formation is also mapped in the valley of the Dry Cimarron in northeastern New Mexico, where it forms a prominent band in the lower parts of the cliffs. The Lytle was the last (youngest) non-marine unit to form in the Denver Basin before the region was fully inundated by the Western Interior Seaway.
While the majority of production has occurred in Cretaceous-aged units, the Paleozoic rocks of the Four Corners Platform have successfully produced from over two-dozen fields from Devonian, Mississippian, and Pennsylvanian-aged units. The Paleozoic units deepen in a northeast direction where they cross from the oil- to the gas-window; subsequently, Paleozoic fields yield gas in the northeast and oil in the southwest. Furthermore, Paleozoic field locations roughly align with the northeast-trending Hogback monocline. Future Paleozoic plays will target natural gas, and these will include untested carbonates in the Central Basin Platform and potentially undiscovered plays in the Four Corners Platform.
In 1958, John Bandimere Sr. purchased a parcel of land on the west side of Denver nestled up against the Hogback leading up to the Rocky Mountains. He and his family began the process of constructing a small but efficient drag strip that was to be used to augment their auto parts business. It also was the fulfillment of a dream of John Sr.'s to provide a safe environment for young people to learn about cars and race them off the streets. In 1988 the Bandimere family made the decision to undergo a much-needed $4 million improvement project, which included a year sabbatical on the national event circuit.
The type section is at Arroyo del Tuerto (Arroyo Pinovetito) where it cuts a slot canyon through Espinaso Ridge. Espinaso Ridge is a hogback produced by the strongly cemented volcaniclastics of the Espinaso Formation, which contrast with the less resistant beds of the underlying Galisteo Formation and overlying Tanos Formation.Stears 1953 Radiometric dating gives an age range of 34.3 +/-0.8 Ma near the base of the formation, 34.6 +/-0.7 Ma near the middle, and 26.9 +/-0.6 my near the top. A basalt flow at the base of the overlying Tanos Formation has an age of 25.1 +/-0.6 Ma. The formation intertongues with the underlying Galisteo Formation but unconformably underlies the Tanos Formation of the Santa Fe Group.
The Kapa Kapa trail across the Owen Stanley divide was a "dank and eerie place, rougher and more precipitous" than the Kokoda Track on which the Australians and Japanese were then fighting. Lead elements of the 126th finally crossed the gap near Mount Obree, which they nicknamed Ghost Mountain, where all of the remaining native porters abandoned the Americans, leaving them to carry their own equipment. On 20 November 1942, after almost 42 days on the trail, crossing exceedingly difficult terrain, including hogback ridges, jungle, and mountainous high- altitude passes, E Company was the first to reach Soputa near the front. The remainder of the battalion trickled in over the next few days.
Hogbacks are recumbent stone monuments found across Scotland and Northern England that date to the 10th – 11th centuries AD; the term ‘hogback’ was established prior to 1885 to describe the characteristic curved ridge of the monument. Hogbacks are often decorated with rows of tegulation on the broad faces and each end often sports stylised or naturalistic beasts, though there is substantial variation on these traits from monument to monument. The tegulation has led many to argue that hogbacks are meant to emulate a house-shape, specifically Scandinavian long houses. Five hogbacks are housed at Govan Old, the largest collection of hogbacks in Scotland; four of these are the largest known hogbacks in all of Great Britain.
Opposite the cricket pitch stands Hutchins Barn, a 16th-century timbered house with a minstrels' gallery. Eghams Farm, built in Tudor times, is a private residence and stands on a path leading to Hogback Wood.History on Line Knotty Green, Accessed 2 July 2015 In one corner of the small recreation area adjoining the cricket pitch, there is an old dew pond formerly used for sheep dipping and reputed to have been in existence for 400 years. The development that followed the arrival of the railway in Beaconsfield in 1906 increased the population of the parish as a whole by nearly 50 per cent in five years, but it was confined to the Penn Road and Forty Green Road.
The town of Leyden consists of a collection of square frame homes with pyramidal roofs that were originally red trimmed in white. It was named for pioneer miner brothers Michael, Martin and John Leyden, who discovered the original Leyden mine in the hogback ridge to the west, where Michael and Martin died in 1866 and 1870, respectively. At its height, the town of Leyden included these homes as well as the company store, school, boarding house, saloon, and Presbyterian chapel. The store still stands at the southeast corner of 82nd and Quaker, while the school is the easternmost house on the hillside to the north, and the foreman's house stands next door to its west.
The principal change was the shortcut from the Virgin River where the road ascended to Mormon Mesa at Virgin Hill, crossed the mesa to the Muddy River and its crossing at California Wash. This saved the longer route to Halfway Wash through the quicksands along the Virgin River. The later immigrants and the Mormon colonists of San Bernardino, in the early 1850s found a better route through Cajon Pass along a hogback in the western side of the Upper Cajon Pass overlooked by Baldy Mesa. At the same time along the Mormon Road were being seeded many of the Mormon settlements that developed into towns and cities of modern Utah, Arizona, Nevada and Southern California.
First h/b edition Cover art by Arthur Orbaan Silver Canyon is a novel written by Louis L'Amour set in south-central Utah Territory in 1881. It was originally published in a shorter version, named Riders of the Dawn, in the magazine Giant Western in June 1951. It then was published in hardback in 1956 by Avalon Books and in paperback by Bantam Books in 1957. Bantam Books republished the short version in 1986 along with two other stories ( The trail to crazy man which was expanded later to Crossfire Trail and Showdown on the Hogback, the original version of Showdown at Yellow Butte) under the title The Trail to Crazy Man.
Alexander Rooney came west in 1859 seeking an opportunity.Rooney Ranch; author unknown; National Register of Historic Places Inventory – Nomination Form; United States Department of the Interior, National Park Service; Washington, D.C.; February 13, 1975 He did a variety work to earn his keep from stone masonry (Central City, the Masonic Lodge), cartage of lumber and other supplies to the mining camps around Denver and South Park, to a dairy farm. He found the high altitude uncomfortable, so he sought out winter pasture at lower elevations for his cattle. In the fall of 1861 he found what he was looking for along the eastern edge of the hogback, between the mountains and the plains.
The 18-mile (29-kilometer) northern section of Ganargua Creek, known as the "Lower" on watershed documents, begins in the Wayne County town of Palmyra at a spillway off the Erie Canal near Swifts Landing Park west of Galloway Road along NY Route 31. Access to the area can be made from the Erie Canalway Trail via Swifts Landing Park on Hogback Road. Ganargua Creek runs northeast towards the community of East Palmyra and into the town of Arcadia, following the CSX Transportation railroad line. It will pass just north of the village of Newark and continue northeast along the Ontario Midland Railroad line to just south of the community of Fairville Station at Norsen Bridge Park.
WSPA-TV, virtual channel 7 (VHF digital channel 11), is a CBS-affiliated television station licensed to Spartanburg, South Carolina, United States, serving Upstate South Carolina and Western North Carolina. The station is owned by Nexstar Media Group, as part of a duopoly with Asheville, North Carolina-licensed CW affiliate WYCW (channel 62). The two stations share studios on International Drive (next to the I-26 and I-85 Business/Veterans Parkway interchange) in Spartanburg and transmitter facilities on Hogback Mountain in northeastern Greenville County (southwest of Tryon, North Carolina). WSPA-TV is the only station in the market that is headquartered in Spartanburg, and in turn tends to focus its local news stories on that city, with a secondary emphasis on Greenville and Asheville.
The Coldwater Sandstone (or Coldwater Formation) is a sedimentary geologic unit of Eocene age found in Southern California, primarily in and south of the Santa Ynez Mountains of Santa Barbara County, and east into Ventura County. It consists primarily of massive arkosic sandstone with some siltstone and shale. Being exceptionally resistant to erosion, outcrops of the Coldwater form some of the most dramatic terrain on the south slope of the Santa Ynez Mountains, with immense white sculpted slabs forming peaks, hogback ridges, and sheer cliff faces.Minor, S.A., Kellogg, K.S., Stanley, R.G., Gurrola, L.D., Keller, E.A., and Brandt, T.R., 2009, Geologic Map of the Santa Barbara Coastal Plain Area, Santa Barbara County, California: U.S. Geological Survey Scientific Investigations Map 3001, scale 1:25,000, 1 sheet, pamphlet, 38 p.
East-West cross-section through the Denver Basin The basin consists of a large asymmetric syncline of Paleozoic, Mesozoic, and Cenozoic sedimentary rock layers, trending north to south along the east side of the Front Range from the vicinity of Pueblo northward into Wyoming. The basin is deepest near Denver, where it reaches a depth of approximately 13,000 ft (3900 m) below the surface. The basin is strongly asymmetric: the Dakota Sandstone outcrops in a "hog-back" ridge near Morrison a few miles west of Denver, reaches its maximum depth beneath Denver, then ascends very gradually to its eastern outcrop in central Kansas. The Dakota hogback exposes Dakota Sandstone overlying and protecting the Morrison Formation beneath and to the west.
Scientists hypothesize that the shallow angle of the subducting plate increased the friction and other interactions with the thick continental mass above it. Tremendous thrusts piled sheets of crust on top of each other, building the broad, high Rocky Mountain range. Tilted slabs of sedimentary rock in Roxborough State Park near Denver The current southern Rockies were forced upwards through the layers of Pennsylvanian and Permian sedimentary remnants of the Ancestral Rocky Mountains. Such sedimentary remnants were often tilted at steep angles along the flanks of the modern range; they are now visible in many places throughout the Rockies, and are shown along the Dakota Hogback, an early Cretaceous sandstone formation running along the eastern flank of the modern Rockies.
Originally, Tempe Butte was part of a series of horizontal layers, but the strata has been tilted associated with the formation of South Mountain, and millennia of erosion has created the distinctive hogback of resistant andesite, over sedimentary deposits and rhyolite beds. Despite intensive development, the butte and its immediate surroundings continue to support a variety of native vegetation, including saguaro, buckhorn cholla, barrel cactus, creosote bush, wolfberry, mormon tea, sweetbush, desert lavender, California buckwheat catclaw acacia, palo verde and mesquite. Springtime annuals include Coulter's and Arizona lupine (Lupinus sparsiflorus and Lupinus arizonicus), Coulter's globemallow (Sphaeralcea coulteri), popcorn flowers (Cryptantha), fiddlenecks (Amsinckia), heliotropes (Phacelia), blonde plantain (Plantago ovata) and others. During the summer wild buckwheat (Eriogonum deflexum) blooms, leaving behind a "skeleton" in the fall.
To the east of the river are several mountains in the Upper Bald Hills, including Northfield Mountain, Brush Mountain (the highest point in town), Beers Mountain, South Mountain, Notch Mountain and Hogback Mountain (along the New Hampshire border). The southeast corner of the town is protected as part of the Northfield State Forest, with part of the northwest corner protected as part of Satan's Kingdom Wildlife Management Area. Most of the inhabited areas in town lie along the Connecticut River, and the town's main villages include East Northfield, Mount Hermon Station, Gill Station, Northfield Farms, and Sky Farm (between Brush Mountain and Northfield State Forest). The town is also home to a cross- country skiing area at Northfield Mountain, which is also traversed by the Metacomet-Monadnock Trail.
The area is predominately generally horizontal sandstone beds with some shale sequences of late Cretaceous and early Cenozoic age. A few areas of the section also have abundant volcanic necks and buttes, but due to the arid weather and soft sandstone, many of the rock formations of the area have eroded to form distinctive features of long cuestas, shallow canyons and valleys, narrow fan terraces, undulating plateaus, isolated mesas, steep hills, and some shale badlands. ;San Juan Basin Near the Four Corners area is a steeply tilted monocline known as The Hogback, which trends southwestward from where the San Juan River enters the area. Here the San Juan River flows into an area known as the San Juan Basin, where the western San Juan Basin is typified by exposures of the Fruitland and Menefee Formations.
Early rail bridges in Queensland were half-through or deck-type lattice girders with through hogback central spans until the 1893 after which the Whipple truss (double intersection through Pratt truss) was used for strength until the introduction of the through Pratt truss in 1897. For the next two decades many of Queensland's rail bridges were of the through Pratt design, including the half-through Pratt for lighter loads (introduced 1909), which features top and bottom chords connected by vertical and diagonal members but no portal or lateral bracing between the two parallel trusses on either side of the rail deck. The Warren truss was introduced later. During the interwar period the rapid increase in production in the Mary Valley made a significant contribution to the Gympie region's status as one of Queensland's most productive dairy areas.
The Narrows is the name given to a geological feature located east of Benjamin in Knox County, Texas. It is a narrow crest running east-to-west along a hogback dividing the watershed of the Wichita River to the north from that of the Brazos River to the south. That is, precipitation falling to the north of the crest will flow into the Wichita River, and thence into the Red River and ultimately the Mississippi, while precipitation falling to the south will flow into the Brazos and then directly into the Gulf of Mexico. Before white settlers arrived in the area, buffalo were drawn to the spot due to the presence of buffalo grass and fresh springs, with the result that the area was known as prime hunting ground to several tribes of Indians, including the Comanche, Wichita, Kiowa, Apache, Seminole, and Tonkawa.
The settlement encompassed land originally belonging to Tséheya Begay. According to one of Shelton's early reports, Navajo had been irrigating the land for many years, with 275 farms drawing water from approximately 25 ditches between the Shiprock area and Farmington. Under Shelton, the agency expanded the irrigation system and developed a dairy herd as part of its agricultural progra; a sawmill near Sanostee and coal mine in the Hogback area were also developed. Early buildings in Shiprock were constructed of log and adobe, but brick replaced these materials after the disastrous flood of 1912. The superintendent was known as a disciplinarian who was ruthless in his prosecution of “moral lapses,” but is said to have been generally respected throughout the region, particularly for his efforts in adding the Utah- Colorado extension to the main Navajo Reservation.
From Lisle to its western end, NY 79 almost exactly follows the Catskill Turnpike, originally maintained by the Susquehanna and Bath Turnpike Company, which also maintained the Catskill Turnpike east to Bainbridge along NY 206, and east along local roads and NY 54 to Bath. The only notable deviations are local, for easier grades, including along the "hogback" eskers near Center Lisle, and the westbound climb out of Ithaca as a looping Hector Street in place of the original straight climb from halfway up that street (still visible as a right-of-way).The Catskill Turnpike in Stage Coach and Tavern Days NY 79 was assigned as part of the 1930 renumbering of state highways in New York. It initially began at NY 15 (modern NY 96) in Trumansburg and ended at the Pennsylvania state line south of the village of Windsor.
SR-12, as seen from the Head of the Rocks overlook Proceeding west to east for 122 miles (nearly 200 km), the highway starts south of Panguitch at an intersection with US-89, crosses part of Dixie National Forest and Bryce Canyon National Park, continues through the small towns of Tropic, Cannonville, and Henrieville. It crosses various parts of Grand Staircase-Escalante National Monument (GS-ENM), continues northeast through Escalante and over the Escalante River, then over the Hogback, a narrow ridge with no guardrails or shoulders and steep drop-offs on each side. It then proceeds north through more of GS-ENM, Boulder, the Aquarius Plateau, Grover, ending in Torrey at an intersection with SR-24, five miles (8 km) west of Capitol Reef National Park. The long portion of the highway that ascends and descends Boulder Mountain on the Aquarius Plateau is known as Boulder Mountain Highway.
Prior to the American Civil War, Flowers owned and operated three river boats along the Ohio River carrying passengers between Marietta, Ohio and St. Louis, Missouri. After two of his boats were destroyed in a sudden storm, he took the remaining boat and sailed down the Ohio to St. Louis, then up the Missouri River to Kansas City, Kansas, where he settled with his family in Wyandotte (now part of Kansas City). In 1873 he organized the Wyandotte Colony, a party of settlers, and led them west to the Colorado Territory to settle at the Union Colony at Greeley, which had been founded three years early as a religiously-oriented agricultural cooperative. Flowers was not contented at the Union Colony, however, and he relocated later that year upstream on the Cache la Poudre River to just west of Fort Collins, in an area just west of the Dakota Hogback known as Pleasant Valley.
An abundance of archaeological sites, attests to the valley's attraction for the earliest inhabitants of the area. They frequented the area for its abundant resources, including shelter under the many bedrock monoliths scattered across the valley, lithic materials for chipped stone tools, and edible plants and animals. West of the valley, the arkosic sandstones of the Pennsylvanian Fountain formation lie unconformably upon uplifted Precambrian metamorphic rocks of the Front Range (Rathbun 1997:21) . Although mostly covered by recent to pre-Wisconsin alluvium, the Fountain formation forms southwest facing escarpments, or monoliths, with undercut shelters or caves (Rathbun 1997:21), many of which were inhabited by prehistoric peoples. The elevation of the site is approximately 1878 m (6160 ft.) above mean sea level. Elevations surrounding the site range from about 1828 m (6000 ft.) in the Dutch Creek water gap to 1992 m (6536 ft.) on the highest point of the Dakota hogback ridge.
China Head's name is thought by some to have to do with a conical-shaped hill atop the ridge visible from the Fraser, but the name may have to do with long-established Lillooet entrepreneur Cheng Won, who owned a hog ranch on Leon Creek, another valley south and "Wo Hing General Store" in Lillooet. The term "head" in 19th-century frontier usage was a synonym for mountain or ridge or headland, and not meant as a reference to a head. Due south of it is the isolated massif of Yalakom Mountain 2424 m (7953 ft), which is one of the highest in the range and remains a redoubt of mountain sheep and other big game, and historically was part of a long-standing wildlife preserve. East of Yalakom Mountain is Hogback Mountain 2149 m (7051 ft), whose name is not descriptive but concerns Cheng Won's hog ranch on its shoulders from which the pigs would run wild onto the mountain.

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