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Deep Creek Range
The Deep Creek Range, (often refereed to as the Deep Creek Mountains (Goshute: Pi'a-roi-ya-bi), are a mountain range in the Great Basin located in extreme western Tooele and Juab counties in Utah, United States. The range trends north-south (with a curl to the west at the southern end, 16% of range in White Pine County, Nevada), and is composed of granite in its central highest portion. The valley to the east is Snake Valley, and to the west is Deep Creek Valley. Nearby communities include Callao, Utah to the east and the community of Ibapah and the lands of the Confederated Tribes of the Goshute Reservation to the west. The highest point in the Deep Creek Range is Ibapah Peak, an ultra prominent peak, which rises to . Other peaks include Haystack Peak at and Red Mountain at . The range is the source of several perennial streams and supports a diverse coniferous forest, with an "island" of alpine tundra on the highest summits. The range has a vertical relief of above the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or '' granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is near ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ibapah
Ibapah ( ) is a small unincorporated community in far western Tooele County, Utah, United States, near the Nevada state line. Description The settlement is located near the Deep Creek Mountains. The site was originally established in 1859 by Mormon missionaries sent to teach the local Native Americans farming methods. A Pony Express station operated here in 1860 and 1861, and the town was on an early alignment of the Lincoln Highway. A post office operated here from 1883 to 1980. Ibapah is currently inhabited mostly by Goshute people, with scattered farmlands and a trading post belonging to more recent settlers. The community is the headquarters of the Confederated Tribes of the Goshute Reservation, a federally recognized tribe. Originally named Deep Creek for a creek of the same name in the area, the name was later changed to ''Ibapah'', an anglicized form of the Goshute The Goshutes are a tribe of Western Shoshone Native Americans. There are two federally recognized G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges 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 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, 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: di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of The Great Basin
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] |
Great Salt Lake Desert
The Great Salt Lake Desert (colloquially referred to as the West Desert) is a large dry lake in northern Utah, United States, between the Great Salt Lake and the Nevada border. It is a subregion of the larger Great Basin Desert, and noted for white evaporite Lake Bonneville salt deposits including the Bonneville Salt Flats. Description Several small mountain ranges occupy the edges of the desert, such as the Cedar Mountains, Lakeside Mountains, Silver Island Mountains, Hogup Mountains, Grassy Mountains, and Newfoundland Mountains. On the western edge of the desert, just across the border in Nevada, stands Pilot Peak in the Pilot Range. The desert is cool during the winter and includes unusual plants adapted to the dry conditions. Most of the desert receives less than of annual precipitation. The salt crust covering the desert reforms yearly when the rain evaporates. The military's Utah Test and Training Range is in the northern portion of the desert. The lowest part of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Tundra
Alpine tundra is a type of natural region or biome that does not contain trees because it is at high elevation, with an associated harsh climate. As the latitude of a location approaches the poles, the threshold elevation for alpine tundra gets lower until it reaches sea level, and alpine tundra merges with polar tundra. The high elevation causes an adverse climate, which is too cold and windy to support tree growth. Alpine tundra transitions to sub-alpine forests below the tree line; stunted forests occurring at the forest-tundra ecotone are known as '' Krummholz''. With increasing elevation it ends at the snow line where snow and ice persist through summer. Alpine tundra occurs in mountains worldwide. The flora of the alpine tundra is characterized by dwarf shrubs close to the ground. The cold climate of the alpine tundra is caused by adiabatic cooling of air, and is similar to polar climate. Geography Alpine tundra occurs at high enough altitude at any latitude. Por ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coniferous Forest
Conifers are a group of cone-bearing seed plants, a subset of gymnosperms. Scientifically, they make up the division Pinophyta (), also known as Coniferophyta () or Coniferae. The division contains a single extant class, Pinopsida. All extant conifers are perennial woody plants with secondary growth. The great majority are trees, though a few are shrubs. Examples include cedars, Douglas-firs, cypresses, firs, junipers, kauri, larches, pines, hemlocks, redwoods, spruces, and yews.Campbell, Reece, "Phylum Coniferophyta". Biology. 7th. 2005. Print. P. 595 As of 1998, the division Pinophyta was estimated to contain eight families, 68 genera, and 629 living species. Although the total number of species is relatively small, conifers are ecologically important. They are the dominant plants over large areas of land, most notably the taiga of the Northern Hemisphere, but also in similar cool climates in mountains further south. Boreal conifers have many wintertime adaptations ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haystack Peak
Haystack Peak is a mountain summit located in Juab County, Utah, United States. Description Haystack Peak is the second-highest summit in the Deep Creek Mountains which are a subset of the Great Basin Ranges, and it is set on land administered by the Bureau of Land Management. The Dugway Proving Ground is northeast of the peak and line parent Ibapah Peak is 1.5 mile to the southwest. Topographic relief is significant as the east aspect rises in six miles, and the west aspect rises over in two miles. Bristlecone pine can be found on the peak's slopes, as well as spruce, fir, and aspen. Precipitation runoff from the mountain's west slope drains into Sams Creek, the northwest slope drains into Indian Farm Creek, and the south slope is drained by Red Cedar Creek. This landform's toponym was officially adopted in 1974 by the U.S. Board on Geographic Names. Climate Haystack Peak is set in the Great Basin Desert which has hot summers and cold winters. The desert is an exampl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ultra Prominent Peak
An ultra-prominent peak, or Ultra for short, is a mountain summit with a topographic prominence of or more; it is also called a P1500. The prominence of a peak is the minimum height of climb to the summit on any route from a higher peak, or from sea level if there is no higher peak. There are approximately 1,524 such peaks on Earth. Some well-known peaks, such as the Matterhorn and Eiger, are not Ultras because they are connected to higher mountains by high cols and therefore do not achieve enough topographic prominence. The term "Ultra" originated with earth scientist Steve Fry, from his studies of the prominence of peaks in Washington in the 1980s. His original term was "ultra major mountain", referring to peaks with at least of prominence. Distribution Currently, 1,518 Ultras have been identified above sea level: 639 in Asia, 356 in North America, 209 in South America, 120 in Europe (including 12 in the Caucasus), 84 in Africa, 69 in Oceania, and 41 in Antarctica. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Confederated Tribes Of The Goshute Reservation
The Confederated Tribes of the Goshute Reservation is located in Juab County, Utah, Tooele County, Utah, and White Pine County, Nevada, United States. It is one of two federally recognized tribes of Goshute people, the other being the Skull Valley Band of Goshute Indians of Utah. Government The tribe's headquarters is in Ibapah, Utah, which is an English adaption form a native Goshute term, either from Ai'ba-pa (one name of the last chief of the tribe who was also known under the common chieftain name ''ta'bi'') or from Ai-bim-pa / Ai'bĭm-pa ("White Clay Water" referring to the nearby Deep Creek). Their own name is Ai'bĭm-pa / Aipimpaa Newe ("People of Deep Creek Valley"). Reservation Approximately 200 tribal members live on the reservation, which is located in White Pine County in eastern Nevada Nevada ( ; ) is a state in the Western region of the United States. It is bordered by Oregon to the northwest, Idaho to the northeast, California to the west, Arizona to t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Callao, Utah
Callao ( ) is a community in northern Snake Valley, along the border of Juab and Tooele counties, Utah, United States. Description The community was part of the original Pony Express overland route, and was first called Willow Springs in 1860. E. W. Tripp, his wife, and their son were the first to establish residence there, in 1870. In 1895 it was decided that ''Willow Springs'' was too common a name, and a new name would be chosen. The name ''Callao'' was chosen because of a resemblance to Callao, Peru, suggested by an old grizzled 1890s prospector in the region who was working out of Gold Hill to the north. It is unknown how the pronunciation changed from the Spanish . Climate According to the Köppen Climate Classification system, Callao has a semi-arid climate A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ibapah Peak
Ibapah Peak is a summit in Juab County, Utah in the United States. It is the highest point of the Deep Creek Range and is located less than east of the Utah-Nevada border, and about northwest of the town of Trout Creek, Utah. With a topographic prominence of it is the eighth-most prominent summit in Utah. See also *List of mountain peaks of Utah *List of the most prominent summits of the United States The following sortable table comprises the 200 most topographically prominent mountain peaks of the United States of America. The summit of a mountain or hill may be measured in three principal ways: #The topographic elevation of a summit me ... References External linksIbapah Peakat SummitPost {{Utah-geo-stub Mountains of Utah Mountains of Juab County, Utah North American 3000 m summits Mountains of the Great Basin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
