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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] |
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] |
Snake Creek (Provo River Tributary)
Snake Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed November 9, 2020 southeastward-flowing stream tributary to the middle section of the Provo River in Wasatch County, Utah. History Snake Creek was named for a nest of rattlesnakes in a dry “hot pots". Hot pots are formed by natural hot-water springs that create crater-like depressions in mounds of tufa (calcium carbonate). The snakes were seen as pests and eradicated, and the dry pot became a limestone quarry. Snake Creek Canyon saw significant mining activity beginning in 1894 when a reporter wrote of a “handsome specimen of copper” from the head of Snake Creek Canyon. In 1897, the Steamboat Company began work in the Snake Creek headwaters. Watershed and Course Snake Creek originates on the southeastern slope of Sunset Peak, about south of Brighton. and flows southeast through Snake Creek Canyon, receiving Lavina Creek (from the left heading downs ... [...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] |
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] |
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] |
Midway, Utah
Midway is a city in northwestern Wasatch County, Utah, United States. It is located in the Heber Valley, approximately west of Heber City and southeast of Salt Lake City, on the opposite side of the Wasatch Mountains. The population was 3,845 at the 2010 census. History A post office called Midway has been in operation since 1864. The town was so named for its central location in an agricultural district. Geography According to the United States Census Bureau, the city has a total area of 3.3 square miles (8.7 km2), all land. The region in which Midway sits is known as the Wasatch Back. Midway is bisected from north to south by Snake Creek, which includes the Midway Fish Hatchery just before the creek joins the middle section of the Provo River above Deer Creek Reservoir. Climate This climatic region is typified by large seasonal temperature differences, with warm to hot summers and cold (sometimes severely cold) winters. According to the Köppen Climate Classi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Baldy (Salt Lake County, Utah)
Mount Baldy is an summit on the boundary that Salt Lake County shares with Utah County, in Utah, United States. Description Mount Baldy is located southeast of downtown Salt Lake City at the Alta Ski Area in the Wasatch–Cache National Forest. The peak is part of the Wasatch Range which is a subrange of the Rocky Mountains. Precipitation runoff from the mountain's north slope drains to Little Cottonwood Creek, whereas the south slope drains into headwaters of the American Fork River. Topographic relief is significant as the summit rises approximately 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. Climate Mount Baldy has a subarctic climate (Köppen ''Dfc''), bordering on an Alpine climate (Köppen ''ET''), with long, cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brighton Ski Resort
Brighton Ski Resort is a ski area located in Big Cottonwood Canyon in Brighton, Utah, United States, about from downtown Salt Lake City. It is owned and operated by Boyne Resorts. Description Brighton Ski Resort was the first ski resort in Utah, and one of the first in the United States. Brighton was started in 1936 when members of the Alpine Ski Club built a rope tow from wire and an old elevator motor. The resort was named for Thomas W. Brighton, who is credited with constructing the first buildings in the area. In 1943, Zane Doyle and Willard Jensen purchased the T-bar from K Smith. In 1954 when there was talk of expansion, Willard insisted that going out on a limb to build a double chair lift instead of another T-bar was worth the risk. Those important changes were able to come about when in 1955 Zane's brother-in-law, Dean L Jensen sold his Idaho business and joined Willard and Zane to build the first double chair lift, Mt Majestic, which was constructed parallel to the o ... [...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] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'', ''Dwd'' and ''Dsd''. Description This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below and in summer, the temperature may exceed . However, the summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least to fall into this category of climate, and the coldest month should a ... [...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] |
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