Mount Raymond (Utah)
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Mount Raymond (Utah)
Mount Raymond is a mountain summit located in Salt Lake County, Utah, United States. Description Mount Raymond is set along the boundary of the Mount Olympus Wilderness on land managed by Wasatch National Forest, with Salt Lake City 11 miles to the west and Park City 11 miles to the east. It is situated in the Wasatch Range which is a subset of the Rocky Mountains. Neighbors include Mount Olympus four miles to the west, Kesler Peak three miles southeast, and line parent Gobblers Knob is 1.5 mile to the northeast. Precipitation runoff from the mountain's north slope drains to Mill Creek, whereas the south slope drains to Big Cottonwood Creek. Topographic relief is significant as the summit rises above Big Cottonwood Canyon in 1.5 mile. This mountain's toponym has been officially adopted by the 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 In ...
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Gobblers Knob (Utah)
Gobblers Knob is a mountain summit located in Salt Lake County, Utah, United States. Description Gobblers Knob is the highest point in the Mount Olympus Wilderness, and is set on land managed by Wasatch National Forest. This peak is situated in the Wasatch Range which is a subset of the Rocky Mountains, and with Salt Lake City 12 miles to the west and Park City 10 miles to the east, it is a popular hiking destination. Neighbors include Mount Raymond 1.5 mile to the southwest and Kesler Peak is 3.2 miles to the south. Precipitation runoff from the mountain's north slope drains to Mill Creek, whereas the south slope drains to Big Cottonwood Creek. Topographic relief is significant as the summit rises above Mill Creek Canyon in 1.5 mile. Climate History This mountain's toponym was officially adopted in 1964 by the United States Board on Geographic Names.United States Board on Geographic Names (1964), ''Decisions on Names in the United States, Decision ...
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Mount Olympus (Utah)
Mount Olympus in the U.S. state of Utah is one of the most prominent and recognizable mountains viewable from practically every location in the Salt Lake Valley. Mount Olympus is not the tallest peak along the Wasatch Front, but its unusual form and location make it a popular hiking destination for locals. The mountain is situated immediately east of the center of the Salt Lake Valley (due east from Murray and Taylorsville). Distinctive features of the mountain are its twin peaks and other outcroppings, the highest of which is called "Summit Peak" and which towers above the valley to an elevation of . Thus, the peak looms about above the valley floor. Hiking Because of its proximity, visibility, and accessibility to a large metropolitan area, Mount Olympus has been a popular hiking destination for the residents of the Salt Lake Valley for many years. Most hikers reach the summit via the Mount Olympus Trail, which is a steep hike from the mountain base and stretches approximate ...
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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 or geography. Etymology The word ''north'' is related to the Old High German ''nord'', both descending from the 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 Greek '' boreas'' "north wind, north", which, according to Ovid, was personified as the wind-god 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 word ''Arctic''. Other languages have other derivations. For example, in Lezgian, ''kefer'' can mean b ...
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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 ...
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Mountains 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 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 ...
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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 ques ...
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Topographic Relief
Terrain or relief (also topographical relief) involves the vertical and horizontal dimensions of land surface. The term bathymetry is used to describe underwater relief, while hypsometry studies terrain relative to sea level. The Latin word (the root of ''terrain'') means "earth." In physical geography, terrain is the lay of the land. This is usually expressed in terms of the elevation, slope, and orientation of terrain features. Terrain affects surface water flow and distribution. Over a large area, it can affect weather and climate patterns. Importance The understanding of terrain is critical for many reasons: * The terrain of a region largely determines its suitability for human settlement: flatter alluvial plains tend to have better farming soils than steeper, rockier uplands. * In terms of environmental quality, agriculture, hydrology and other interdisciplinary sciences; understanding the terrain of an area assists the understanding of watershed boundaries, drai ...
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Big Cottonwood Creek
Big Cottonwood Creek is one of the largest streams entering Salt Lake Valley from the east from the Wasatch Mountains. The creek flows through the Big Cottonwood Canyon in a westerly direction until it emerges into Salt Lake Valley about from its highest source. Thence its course is northwesterly through Cottonwood Heights, Utah, Cottonwood Heights, Holladay, Utah, Holladay, and Murray, Utah until it empties into the Jordan River (Utah), Jordan River about south of Salt Lake City. In the summer, its waters are all used for irrigation purposes. From its source to its original outlet in the Jordan River is about twenty-six miles. Hydrology The creek flows from around at the headwaters to around when it reaches the confluence with the Jordan River. The stream flows northwest as it leaves the headwaters near the Brighton Ski Resort and then travels southwest about halfway down the canyon near Reynolds Gulch. At the base of the canyon, the stream leaves the Uinta-Wasatch-Cache Natio ...
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Surface Runoff
Surface runoff (also known as overland flow) is the flow of water occurring on the ground surface when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is saturated by water to its full capacity, and the rain arrives more quickly than the soil can absorb it. Surface runoff often occurs because impervious areas (such as roofs and pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or man-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. Runoff that occurs on the ground surface before reaching a channel can be a nonpoint source of pollution, as it can carry man-made contaminants or natural forms of pollution (such as rotting leaves). Man-made contaminants in runoff i ...
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Line Parent
A peak's line parent is the closest higher peak on the highest ridge leading away from the peak's "key col". A col is the lowest point on the ridge between two summits and is roughly synonymous with pass, gap, saddle and notch. The highest col of a peak is its key col. If there is more than one ridge which can be followed to a higher peak then the line parent is the peak closest to the key col. Usually, a line parent must meet some prominence criteria, which might vary depending on the author and the location of the peak. There are at least two other kinds of peak parentage. Island parentage, which is also referred to as encirclement or topographic parentage; and source parentage. See also * Topographic prominence In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest contou ... References ...
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Kesler Peak (Wasatch Range)
Kesler Peak is a mountain summit located in Salt Lake County, Utah, United States. Description Kesler Peak is set in the Wasatch Range which is a subset of the Rocky Mountains. It is situated in Big Cottonwood Canyon, on land managed by Wasatch National Forest. Salt Lake City is 13 miles to the northwest and Solitude Mountain Resort is four miles to the east. Neighbors include Mount Raymond three miles to the northwest and Gobblers Knob is 3.2 miles to the north. Precipitation runoff from the mountain's slopes drains to Big Cottonwood Creek. Topographic relief is significant as the summit rises above Big Cottonwood Canyon in 1.5 mile. History The spelling of this mountain's toponym was officially changed in 2008 by the United States Board on Geographic Names. Prior to that it was spelled "Kessler Peak" which appears on older maps, and was also known as "Kessler's Peak" in the early 1900s. This landform is named after Frederick Kesler Frederick Kesler ...
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Park City, Utah
Park City is a city in Utah, United States. The vast majority is in Summit County, and it extends into Wasatch County. It is considered to be part of the Wasatch Back. The city is southeast of downtown Salt Lake City and from Salt Lake City's east edge of Sugar House along Interstate 80. The population was 8,396 at the 2020 census. On average, the tourist population greatly exceeds the number of permanent residents. After a population decline following the shutdown of the area's mining industry, the city rebounded during the 1980s and 1990s through an expansion of its tourism business. the city brings in a yearly average of $529.8 million to the Utah Economy as a tourist hot spot, $80 million of which is attributed to the Sundance Film Festival. The city has two major ski resorts: Deer Valley Resort and Park City Mountain Resort (combined with Canyons Village at Park City) and one minor resort: Woodward Park City (an action sports training and fun center). Both Deer Valley ...
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