|
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] |
Utah
Utah ( , ) is a state in the Mountain West subregion of the Western United States. Utah is a landlocked U.S. state bordered to its east by Colorado, to its northeast by Wyoming, to its north by Idaho, to its south by Arizona, and to its west by Nevada. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin. Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo and Ute. The Spanish were the first Europ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granodiorite
Granodiorite () is a coarse-grained ( phaneritic) intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. The term banatite is sometimes used informally for various rocks ranging from granite to diorite, including granodiorite. Composition According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase. A greater amount of plagioclase would designate the rock as tonalite. Granodiorite is felsic to intermediate in composition. It is the intrusive igneous equivalent of the extrusive igneous dacite. It contains a large amount of sodium (Na) and calcium (Ca) rich plagioclase, potassium feldspar, quartz, and minor amounts of muscovite mica as the lighter colored mineral components. Biotite and amphiboles often in the form of hornblende are more abundant in granodiorite than in granite, giving it a more distinct two-toned or overall darker appeara ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North American 3000 M Summits
North is one of the four compass points or cardinal directions. It is the opposite of south and is perpendicular to east and west. ''North'' is a noun, adjective, or adverb indicating Direction (geometry), direction or geography. Etymology The word ''north'' is etymology, related to the Old High German ''nord'', both descending from the Proto-Indo-European language, Proto-Indo-European unit *''ner-'', meaning "left; below" as north is to left when facing the rising sun. Similarly, the other cardinal directions are also related to the sun's position. The Latin word ''borealis'' comes from the Ancient Greek, Greek ''Anemoi#Boreas, boreas'' "north wind, north", which, according to Ovid, was personified as the wind-god Anemoi#Boreas, Boreas, the father of Calais and Zetes. ''Septentrionalis'' is from ''septentriones'', "the seven plow oxen", a name of ''Ursa Major''. The Greek ἀρκτικός (''arktikós'') is named for the same constellation, and is the source of the English ... [...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 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] |
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] |
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] |
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] |
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] |
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] |
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] |
