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O'Sullivan Peak (Utah)
O'Sullivan Peak, also known as Sunrise Peak, is an mountain summit located in Salt Lake County, Utah, United States. Description O'Sullivan Peak is located southeast of downtown Salt Lake City in the Twin Peaks Wilderness on land managed by Wasatch–Cache National Forest. The peak is set in the Wasatch Range which is a subset of the Rocky Mountains. Precipitation runoff from the mountain's south slope drains to Little Cottonwood Creek, whereas the north slope drains to Big Cottonwood Creek, and both creeks flow west to the Jordan River. Topographic relief is significant as the summit rises above Little Cottonwood Canyon in 1.4 mile (2.25 km). This mountain's toponym was officially adopted in 1978 by the United States Board on Geographic Names to remember Timothy H. O'Sullivan (1840–1882), civil war and western frontier photographer who visited this area as the official photographer of the King Survey and Wheeler Survey The Wheeler Survey, carried out in 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Broads Fork Twin Peaks
The Twin Peaks are a pair of mountain high points located on the Cottonwood Ridge within the Wasatch Range in Salt Lake County, Utah. They are usually referred to as the Broads Fork Twin Peaks, to distinguish them from the nearby American Fork Twin Peaks and Avenues Twin Peaks. Consisting of two sub-peaks, only the eastern peak has the prominence to be considered a true summit, with an elevation of , 2 feet higher than the western subpeak. The eastern peak is the second-highest in Salt Lake County, only behind the nearby American Fork Twins. The Twin Peaks rise directly from the Salt Lake Valley Salt Lake Valley is a valley in Salt Lake County, Utah, Salt Lake County in the north-central portion of the U.S. state of Utah. It contains Salt Lake City, Utah, Salt Lake City and many of its suburbs, notably Murray, Utah, Murray, Sandy, Uta ..., making them easily visible and recognizable. Climate References {{reflist Mountains of Utah Mountains of Salt Lake County, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topographic Relief
Terrain (), alternatively relief or topographical relief, is the dimension and shape of a given surface of land. In physical geography, terrain is the lay of the land. This is usually expressed in terms of the elevation, slope, and orientation of terrain features. Terrain affects surface water flow and distribution. Over a large area, it can affect weather and climate patterns. Bathymetry is the study of underwater relief, while hypsometry studies terrain relative to sea level. Importance The understanding of terrain is critical for many reasons: * The terrain of a region largely determines its suitability for human settlement: flatter alluvial plains tend to have better farming soils than steeper, rockier uplands. * In terms of environmental quality, agriculture, hydrology and other interdisciplinary sciences; understanding the terrain of an area assists the understanding of watershed boundaries, drainage characteristics, drainage systems, groundwater systems, water ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Three-thousanders Of The United States
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term refers to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Andes) it m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Salt Lake County, Utah
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Utah
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are inselberg, isolated summits, but most occur in mountain ranges. mountain formation, Mountains are formed through tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosystems of mountains: different elevations hav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lone Peak (Utah)
Lone Peak is a mountain summit in the Wasatch Range southeast of Salt Lake City, Utah, United States, and the center of the Lone Peak Wilderness, established in 1978. With an elevation of , it is one of the highest peaks in the range and among the most prominent of the Wasatch Front, towering over the Salt Lake City suburb of Draper and easily visible from most of the valley, which makes it a popular destination for hiking and rock climbing. The first person in recorded history to scale the summit of Lone Peak was Richard Bell, Sr. of Riverton, Utah. Bell also led the first recorded climb of the Lone Peak Cirque. He went on to lead several expeditions and taught many alpine guides. Bells Canyon is named for him and is still a common route to the summit. Lone Peak consists almost entirely of quartz monzonite (a granitoid or granite-like rock) of the 30.5 million-year-old Little Cottonwood Stock. Quartzite and limestone are also found in distal locations on the mountain. The high ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Superior
Mount Superior (also known as Superior Peak) is an mountain peak in the Uinta-Wasatch-Cache National Forest in Salt Lake County, Utah, United States. With prominent visibility from Utah State Route 210 in Little Cottonwood Canyon, and being only 35 minutes from downtown Salt Lake City, it is a popular hiking, climbing, and skiing destination. Routes There are many ways to access the summit of Mount Superior, with the two most popular options being via the Cardiff Pass and South Ridge trails. Cardiff Pass The Cardiff Pass trail follows a well-maintained route starting in the town of Alta until it reaches Cardiff Pass. Once the pass has been reached, it skirts around Cardiff Peak along a ridge line to the summit. South Ridge The summit can also be reached via the South Ridge. Considered a 5th class scramble or rock climb, the ascent can be made, depending on ones climbing experience and conditions, free solo Free solo climbing, or free soloing, is a form of rock cli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Big Cottonwood Canyon
Big Cottonwood Canyon is a canyon in the Wasatch Range southeast of Salt Lake City in the U.S. state of Utah. The -long canyon provides hiking, biking, picnicking, rock-climbing, camping, and fishing in the summer. Its two ski resorts, Brighton and Solitude, are popular among skiers and snowboarders. The canyon is accessed by The Big Cottonwood Canyon Scenic Byway (SR-190), which runs its length to Guardsman Pass at the top of the canyon, allowing travel to Park City in the summer months. Hiking to the canyon's mountain lakes is popular, with many trails leading to lakes such as Mary, Martha, and Katherine. The canyon's most popular hiking trail leads to Lakes Blanche, Florence and Lillian. The trail is long and a strenuous hike. Since the canyon was formed by Big Cottonwood Creek, the V-shaped canyon has many impressive rock forms. The canyon is also a frequent destination for Utah Native Plant Society wildflower walks and for University of Utah botanical field trips. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dromedary Peak
Dromedary Peak is an mountain summit located in Salt Lake County, Utah, United States. Description Dromedary Peak is located southeast of downtown Salt Lake City in the Twin Peaks Wilderness on land managed by Wasatch–Cache National Forest. The peak is set in the Wasatch Range which is a subrange of the Rocky Mountains. Precipitation runoff from the mountain's south slope drains to Little Cottonwood Creek, whereas the north slope drains to Big Cottonwood Creek, and both creeks flow west to the Jordan River. Topographic relief is significant as the summit rises above Little Cottonwood Canyon in 1.5 mile (2.4 km). This mountain's toponym has been officially adopted by the United States Board on Geographic Names. The descriptive name is because the peak's shape resembles a dromedary camel when viewed from a certain angle.John W. Van Cott, ''Utah Place Names: A Comprehensive Guide to the Origins of Geographic Names'', University of Utah Press, 1990, , p. 116. See als ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wheeler Survey
The Wheeler Survey, carried out in 1872-1879, was one of the "Four Great Surveys" conducted by the United States government after the Civil War primarily to document the geology and natural resources of the American West. Supervised by First Lieutenant (later Captain) George Montague Wheeler, the Wheeler Survey documented and mapped the United States west of the 100th meridian. The survey team included Lieutenant Montgomery M. Macomb, plus the paleontologists Edward Drinker Cope and Charles Abiathar White as well as the astronomer Miles Rock. Wheeler led early expeditions from 1869 to 1871 in the West, and in 1872 the United States Congress authorized an ambitious plan to map the portion of the United States west of the 100th meridian at a scale of eight miles to the inch. This plan necessitated what became known as the Wheeler Survey. The survey's main goal was to make topographic maps of the southwestern United States. In addition he was to ascertain everything related ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geological Exploration Of The Fortieth Parallel
The Geological Exploration of the Fortieth Parallel was a geological survey made by order of the Secretary of War according to acts of Congress of March 2, 1867, and March 3, 1869, under the direction of Brig. and Bvt. Major General A. A. Humphreys, Chief of Engineers, by Clarence King, U. S. geologist. More commonly known as the Fortieth Parallel Survey, the survey conducted field work from 1867 to 1872, exploring the area along the fortieth parallel north from northeastern California, through Nevada, to eastern Wyoming. Results The results of the survey were published in eight volumes of the Fortieth Parallel Survey: Vol. I. Systematic geology by Clarence King, U. S. Geologist. 1878. xii, 803 pp., and atlas of 12 sheets. Vol. II. Descriptive geology by Arnold Hague and S. F. Emmons. 1877. xiii, 890 pp. Vol. III. Mining industry by James Duncan Hague, with geological contributions by Clarence King. 1870. xv, 647 pp. and atlas of 14 sheets. Vol. IV Part I, Palaeontology. by F. B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States Board On Geographic Names
The United States Board on Geographic Names (BGN) is a Federal government of the United States, federal body operating under the United States Secretary of the Interior. The purpose of the board is to establish and maintain uniform usage of geography, geographic names throughout the federal government of the United States. History Following the American Civil War, more and more American pioneer, American settlers began moving westward, prompting the Federal government of the United States, U.S. federal government to pursue some sort of consistency for referencing landmarks on maps and in official documents. As such, on January 8, 1890, Thomas Corwin Mendenhall, superintendent of the United States Coast and Geodetic Survey Office, wrote to 10 noted geographers "to suggest the organization of a Board made up of representatives from the different Government services interested, to which may be referred any disputed question of geographical orthography." President Benjamin Harrison si ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
