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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] |
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] |
Little Cottonwood Creek (Salt Lake County, Utah)
Little Cottonwood Creek is one of the principal streams entering Salt Lake Valley from the east. The creek rises near the summit of the Wasatch Mountains, a short distance south of the ski resort town of Alta, and flows in a westerly direction through Little Cottonwood Canyon until it emerges into Salt Lake Valley about eleven miles from its source. Thence its course is north westerly through Sandy, Midvale and Murray, Utah until it empties into the Jordan River, about six miles south of Salt Lake City. Its whole length is nearly . The headwaters of Little Cottonwood Creek are in Little Cottonwood Canyon, a glaciated canyon in Uinta-Wasatch-Cache National Forest and the Wasatch and Uinta Mountains eco-region. One of the main tributaries of the creek rises in Cecret Lake, a small sheet of water situated near Alta. The entire Little Cottonwood Creek drainage basin encompasses , ranging in elevation from about . Communities were founded around the creek soon after the pioneer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utah County, Utah
Utah County is the second-most populous county in the U.S. state of Utah. The county seat and largest city is Provo, which is the state's third-largest city, and the largest outside of Salt Lake County. As of the 2020 United States Census, the population was 665,665. Utah County is one of two counties forming the Provo- Orem metropolitan statistical area, and is part of the larger Salt Lake City-Provo-Orem, UT Combined Statistical Area. In 2010, the center of population of Utah was in Utah County, in the city of Saratoga Springs. Utah County is one of the fastest-growing counties in the United States, ranking among the top ten counties in numerical growth. Correspondingly, Provo-Orem is among the top eight metropolitan areas by percentage growth in the country. Utah County is one of seven counties in the United States to have the same name as its state. The other six counties are Arkansas County, Hawaii County, Idaho County, Iowa County, Oklahoma County and New York Cou ... [...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] |
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] |
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] |
Stock (geology)
In geology, a stock is an igneous intrusion that has a surface exposure of less than ,Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, p. 513. . differing from batholiths only in being smaller. A stock has a discordant relationship with the rocks that it intrudes. Many stocks are cupolas of hidden batholiths. Some circular or elliptical stocks may be volcanic plugs, which fill the vents of now extinct volcanoes. A boss is a small stock. Examples * the Alta and Clayton Peak stocks (composed of granodiorite), near Park City, Utah * the Hellroaring Creek and Salal Creek stocks (of granite-granodiorite and quartz monzonite, respectively) in British Columbia, Canada * the Céret stock (of gabbro and diorite) in Pyrénées-Orientales, France * the Parashi stock (of tonalite) in La Guajira Department, Colombia * stocks of syenite Syenite is a coarse-grained intrusive igneous rock with a general composition similar to that of granite, but def ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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