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Sunset Peak (Utah)
Sunset Peak is a summit in Utah, United States. Description Sunset Peak is located southeast of downtown Salt Lake City and south of Brighton, Utah, Brighton in the Wasatch–Cache National Forest. It is set on, and in part forms, the boundary point that is shared by Salt Lake County, Utah, Salt Lake County, Utah County, Utah, Utah County, and Wasatch County, Utah, Wasatch County. The peak is set in the Wasatch Range which is a subrange of the Rocky Mountains. Precipitation runoff from the mountain's north slope drains into headwaters of Big Cottonwood Creek, whereas the east slope drains into headwaters of Snake Creek (Provo River tributary), Snake Creek, and the south slope drains to American Fork Canyon. Topographic relief is significant as the summit rises above Snake Creek in one mile (1.6 km). This mountain's toponym has been officially adopted by the United States Board on Geographic Names, and has been recorded in publications since at least 1915. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sugarloaf Mountain (Utah)
Sugarloaf Mountain ( pt, Pão de Açúcar, ) is a peak situated in Rio de Janeiro, Brazil, at the mouth of Guanabara Bay on a peninsula that juts out into the Atlantic Ocean. Rising above the harbor, the peak is named for its resemblance to the traditional shape of concentrated refined loaf sugar. It is known worldwide for its cableway and panoramic views of the city and beyond. The mountain is one of several monolithic granite and quartz mountains that rise straight from the water's edge around Rio de Janeiro. Geologically, it is considered part of a family of steep-sided rock outcroppings known as non-inselberg bornhardts. The mountain is protected by the Sugarloaf Mountain and Urca Hill Natural Monument, created in 2006. This became part of a World Heritage Site declared by UNESCO in 2012. Origins of the name The name Sugarloaf was coined in the 16th century by the Portuguese during the heyday of sugarcane trade in Brazil. According to historian Vieira Fazenda, block ... [...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 body operating under the United States Secretary of the Interior. The purpose of the board is to establish and maintain uniform usage of geographic names throughout the federal government of the United States. History On January 8, 1890, Thomas Corwin Mendenhall, superintendent of the US 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 signed executive order 28 on September 4, 1890, establishing the ''Board on Geographical Names''. "To this Board shall be referred all unsettled questions concerning geographic names. The decisions of the Board are to be accepted y federal departmentsas the standard authority for such matters." The board was given authority to resolve all unsettled q ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Wasatch County, Utah
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Utah 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 300 metres (1,000 feet) 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Wolverine
Mount Wolverine is a summit in Salt Lake County, Utah, United States. Description Mount Wolverine is located southeast of downtown Salt Lake City between the Alta Ski Area and the Brighton Ski Resort in the 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 north slope drains into headwaters of Big Cottonwood Creek, whereas the south slope drains into headwaters of Little Cottonwood Creek. Topographic relief is significant as the summit rises above Little Cottonwood Canyon in approximately one mile (1.6 km). Mount Wolverine is composed of granodiorite of the igneous Alta stock.Miriam H. Bugden, ''Geology and Scenery of the Central Wasatch Range, Salt Lake and Summit Counties, Utah'', Utah Geological Survey, 1991, , p. 12 This mountain's toponym has been officially adopted by the United States Board on Geographic Names. Climate Mount Wolverine has a subarctic climate (K� ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alta Ski Area
Alta is a ski area in the western United States, located in the town of Alta in the Wasatch Mountains of Utah, in Salt Lake County. With a skiable area of , Alta's base elevation is and rises to for a vertical gain of . One of the oldest ski resorts in the country, it opened its first lift in early 1939. Alta is known for receiving more snow than most Utah resorts, with an average annual snowfall of . Alta is one of three remaining ski resorts in the U.S. that prohibits snowboarders, along with nearby competitor Deer Valley and Vermont's Mad River Glen. History Early History Alta is one of the oldest ski areas in the U.S. and is one of just three ski areas in the U.S. that prohibits snowboarders. Located at the head of Little Cottonwood Canyon in Albion Basin and Collins Gulch, barely from the Great Salt Lake, Alta resides in a unique micro climate characterized by over of high volume, low moisture snowfall annually. Alta Ski Area features long, straight, fall-line ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clayton Peak
Clayton Peak, also known unofficially as Mount Majestic, is a summit on the boundary that Salt Lake County shares with Wasatch County, in Utah, United States. Description Clayton Peak is located southeast of downtown Salt Lake City and southeast of Brighton in the 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 west slope drains into headwaters of Big Cottonwood Creek, whereas the east slope drains to Snake Creek. Topographic relief is significant as the summit rises above Snake Creek in 1.5 mile (2.4 km). From Guardsman Pass, reaching the top involves 2.2 miles (round-trip) of hiking along a portion of the Great Western Trail with 1,015 feet of elevation gain.Greg Witt, ''60 Hikes Within 60 Miles: Salt Lake City'', Menasha Ridge Press, 2012, , p. 145. The summit provides views of the Brighton Lakes area, the Uinta Mountains, Heber Valley, and Mount Timpanogo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Tuscarora (Utah)
Mount Tuscarora is a summit in Salt Lake County, Utah, United States. Description Mount Tuscarora is located southeast of downtown Salt Lake City between the Alta Ski Area and the Brighton Ski Resort in the 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 north slope drains into headwaters of Big Cottonwood Creek, whereas the south slope drains into headwaters of Little Cottonwood Creek. Topographic relief is significant as the summit rises above Lake Mary in one-half mile (0.8 km). Mount Tuscarora is composed of granodiorite of the igneous Alta stock.Miriam H. Bugden, ''Geology and Scenery of the Central Wasatch Range, Salt Lake and Summit Counties, Utah'', Utah Geological Survey, 1991, , p. 12 This mountain's toponym has been officially adopted by the United States Board on Geographic Names. Tuscarora was the chief of the Tuscarora people on the East Coast, but why th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Millicent
Mount Millicent is a summit in Salt Lake County, Utah, United States. Description Mount Millicent is located southeast of downtown Salt Lake City at the Brighton Ski Resort in the 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 slopes drains into headwaters of Big Cottonwood Creek. Topographic relief is significant as the summit rises above Brighton in one mile (1.6 km). The mountain is composed of granodiorite of the igneous Alta stock. This mountain's toponym has been officially adopted by the United States Board on Geographic Names. The mountain was listed and depicted as one of the principal peaks of the Rockies in a book published in 1916.Edwin Legrand Sabin, ''The Pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Climate
Alpine climate is the typical weather ( climate) for elevations above the tree line, where trees fail to grow due to cold. This climate is also referred to as a mountain climate or highland climate. Definition There are multiple definitions of alpine climate. In the Köppen climate classification, the alpine and mountain climates are part of group ''E'', along with the polar climate, where no month has a mean temperature higher than . According to the Holdridge life zone system, there are two mountain climates which prevent tree growth : a) the alpine climate, which occurs when the mean biotemperature of a location is between . The alpine climate in Holdridge system is roughly equivalent to the warmest tundra climates (ET) in the Köppen system. b) the alvar climate, the coldest mountain climate since the biotemperature is between 0 °C and 1.5 °C (biotemperature can never be below 0 °C). It corresponds more or less to the coldest tundra climates and t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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