Kesler Peak (Wasatch Range)
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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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Mount Superior
Mount Superior (also known as Superior Peak) is an mountain peak in the Uinta-Wasatch-Cache National Forest in Salt Lake County, Utah, United States. With prominent visibility from Utah State Route 210 in Little Cottonwood Canyon, and being only 35 minutes from downtown Salt Lake City, it is a popular hiking, climbing, and skiing destination. Routes There are many ways to access the summit of Mount Superior, with the two most popular options being via the Cardiff Pass and South Ridge trails. Cardiff Pass The Cardiff Pass trail follows a well-maintained route starting in the town of Alta until it reaches Cardiff Pass. Once the pass has been reached, it skirts around Cardiff Peak along a ridge line to the summit. South Ridge The summit can also be reached via the South Ridge. Considered a 5th class scramble or rock climb, the ascent can be made, depending on ones climbing experience and conditions, free solo Free solo climbing, or free soloing, is a form of technical ic ...
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Salt Lake City
Salt Lake City (often shortened to Salt Lake and abbreviated as SLC) is the Capital (political), capital and List of cities and towns in Utah, most populous city of Utah, United States. It is the county seat, seat of Salt Lake County, Utah, Salt Lake County, the most populous county in Utah. With a population of 200,133 in 2020, the city is the core of the Salt Lake City metropolitan area, which had a population of 1,257,936 at the 2020 census. Salt Lake City is further situated within a larger metropolis known as the Salt Lake City–Provo–Orem Combined Statistical Area, Salt Lake City–Ogden–Provo Combined Statistical Area, a corridor of contiguous urban and suburban development stretched along a segment of the Wasatch Front, comprising a population of 2,746,164 (as of 2021 estimates), making it the 22nd largest in the nation. It is also the central core of the larger of only two major urban areas located within the Great Basin (the other being Reno, Nevada). Salt Lake C ...
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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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Doughnut Falls
Doughnut Falls is a waterfall A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several wa ... in the Big Cottonwood Canyon near Silver Fork, south of Midvale in Salt Lake County, Utah. Access to Chocolate Falls is from the Mill D Trailhead towards the Jordan Pines picnic area. The waterfall plunges into a pothole that has access under the arch of rock with a view up at the falls falling into the pool. See also * List of waterfalls in Utah References Waterfalls of Utah Landforms of Salt Lake County, Utah {{Utah-geologic-formation-stub ...
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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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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 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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