Giraud Peak
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Giraud Peak
Giraud Peak is a mountain summit located west of the crest of the Sierra Nevada mountain range, in Fresno County, California, Fresno County of northern California, United States. It is situated in the Palisades (California Sierra), Palisades area of northern Kings Canyon National Park, southwest of North Palisade, and southwest of Columbine Peak, the nearest higher neighbor. Giraud Peak ranks as the 258th-highest summit in California. Topographic relief is significant as the west aspect rises above LeConte Canyon in less than two miles. On the direct opposite side of the canyon The Citadel (Sierra Nevada), The Citadel stands guard. The first ascent of the summit was made September 1, 1925, by Norman Clyde via the east arête. Etymology This mountain's name has been officially adopted by the United States Board on Geographic Names. It was probably named for Pierre "Little Pete" Giraud (1874–1907), a shepherd of Inyo County who was made famous in Mary Hunter Austin, Mary Austin ...
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Columbine Peak
Columbine Peak is a 12,662-foot-elevation (3,859 meter) mountain summit located west of the crest of the Sierra Nevada mountain range, in Fresno County of northern California, United States. It is situated between Palisade Basin and Dusy Basin in the Palisades area of northern Kings Canyon National Park. It is west of North Palisade, south of Bishop Pass, and immediately north of Knapsack Pass. This mountain's name has been officially adopted by the United States Board on Geographic Names. The first ascent of the summit was made prior to 1925 by persons unknown. Climate According to the Köppen climate classification system, Columbine Peak is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. As fronts approach, they are forced upward by the peaks, causing them to drop their moisture in the form of rain or snowfall onto the range (orographic lift). Precipitation runoff from this mountain ...
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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 to the ...
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Mountains Of Fresno County, California
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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Langille Peak
Langille Peak is a mountain summit located west of the crest of the Sierra Nevada mountain range, in Fresno County of central California, United States. It is situated in northern Kings Canyon National Park, west-southwest of the community of Big Pine, south of Mount Thompson, southwest of Mount Goode, and east of Black Giant. Topographic relief is significant as the east aspect rises above Le Conte Canyon in less than one mile. The approach to this remote peak is made via the John Muir Trail. History The peak's name (pronounced "Lan'jill") honors Harold Douglas Langille (1874–1954), forest inspector for the General Land Office, Department of the Interior, who visited Sierra Forest Reserve on an inspection tour in 1904. The name was officially adopted by the USGS at the suggestion of Charles Howard Shinn, head ranger of the forest reserve. The first ascent of the summit was made in August 1926 by Nathaniel L. Goodrich, Marjory Hurd, and Dean Peabody, Jr. via the ...
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Mount Shakspere
Mount Shakspere is a 12,174-foot-elevation (3,711 meter) summit located in Fresno County, California, United States. Description The mountain is set four miles west of the crest of the Sierra Nevada mountain range, in the Palisades area of Kings Canyon National Park. It is situated southwest of Middle Palisade, southeast of Giraud Peak, and one mile north-northwest of line parent Observation Peak. Mt. Shakspere ranks as the 384th-highest summit in California, and topographic relief is significant as the summit rises over above Palisade Creek in approximately . The first ascent of the summit was made July 20, 1930, by Francis P. Farquhar, Mary Lou Michaels, Doris Drust, Lorna Kilgariff, and Robert L. Lipman. This mountain's name has been officially adopted by the United States Board on Geographic Names. Climate Mount Shakspere is located in an alpine climate zone. Most weather fronts originate in the Pacific Ocean, and travel east toward the Sierra Nevada mountains. ...
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Mount Goode (California)
Mount Goode is a 13,085-foot-elevation (3,988 meter) mountain summit located on the crest of the Sierra Nevada mountain range in California, United States. It is situated on the shared boundary of Kings Canyon National Park with John Muir Wilderness, and along the common border of Fresno County with Inyo County. It is also approximately one mile west-northwest of Bishop Pass, one mile east-southeast of Mount Johnson, south of Hurd Peak, and west of the community of Big Pine. History This mountain's name and location were officially adopted in 1926 by the U.S. Board on Geographic Names based on a recommendation by the Sierra Club. Prior to 1926, the USGS placed Mount Goode at the location of Black Giant. The name commemorates Richard Urquhart Goode (1858–1903), geographer for the United States Geological Survey, in charge of the Pacific Division, Topographic Branch. The first ascent of the peak was made July 16, 1939, by Chester Versteeg, a prominent Sierra Club member. Cl ...
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List Of Mountain Peaks Of California
This article comprises three sortable tables of major mountain peaksThis article defines a significant summit as a summit with at least of topographic prominence, and a major summit as a summit with at least of topographic prominence. All summits in this article have at least 500 meters of topographic prominence. An ultra-prominent summit is a summit with at least of topographic prominence. of the U.S. State of California. The summit of a mountain or hill may be measured in three principal ways: #The topographic elevation of a summit measures the height of the summit above a geodetic sea level.All elevations in this article include an elevation adjustment from the National Geodetic Vertical Datum of 1929 (NGVD 29) to the North American Vertical Datum of 1988 (NAVD 88). For further information, please see this United States National Geodetic Surveybr>noteIf the elevation or prominence of a summit is calculated as a range of values, the arithmetic mean is shown. T ...
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Devils Crags
A devil is the personification of evil as it is conceived in many and various cultures and religious traditions. Devil or Devils may also refer to: * Satan * Devil in Christianity * Demon * Folk devil Art, entertainment, and media Film and television * ''The Devil'' (1908 film), a 1908 film directed by D. W. Griffith * ''The Devil'' (1915 film), an American film starring Bessie Barriscale * ''The Devil'' (1918 Hungarian film), a Hungarian film directed by Michael Curtiz * ''The Devil'' (1918 German film), a German silent mystery film * ''The Devil'' (1921 film), an American film starring George Arliss * '' To Bed or Not to Bed'' (also known as ''The Devil''), a 1963 Italian film * ''The Devils'' (film), a 1971 British film directed by Ken Russell * ''The Devil'' (1972 film), a Polish film * ''The Devil'' (TV series), a 2007 South Korean television series ** ''Devil'' (TV series), a 2008 Japanese television series remake of the South Korean series * ''Devil'' (2010 f ...
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Middle Fork Kings River
The Middle Fork Kings River is a tributary of the Kings River in Kings Canyon National Park, California, in the southern Sierra Nevada. Draining – almost all of it wilderness – the Middle Fork is one of the largest wholly undeveloped watersheds in the state, with no dams or paved roads within its basin. The entire length of the Middle Fork is designated a National Wild and Scenic River. Course The Middle Fork originates at Helen Lake in the high Sierra, near Muir Pass in Kings Canyon National Park. From its headwaters at above sea level, it descends rapidly east down Le Conte Canyon, turning south at Big Pete Meadow. It passes the Le Conte Ranger Station and receives Dusy Creek from the east and then the much larger Palisade Creek, also from the east, a short distance downstream. Flowing south, it enters a narrower canyon where it drops over a waterfall known as Devil's Washbowl. It receives Cartridge Creek from the east, then turns southwest through Simpson Meadow, a broad ...
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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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Orographic Lift
Orographic lift occurs when an air mass is forced from a low elevation to a higher elevation as it moves over rising terrain. As the air mass gains altitude it quickly cools down adiabatically, which can raise the relative humidity to 100% and create clouds and, under the right conditions, precipitation. Orographic lifting can have a number of effects, including precipitation, rain shadowing, leeward winds, and associated clouds. Precipitation Precipitation induced by orographic lift occurs in many places throughout the world. Examples include: * The Mogollon Rim in central Arizona * The western slope of the Sierra Nevada range in California * The mountains near Baja California North – specifically La Bocana to Laguna Hanson. * The windward slopes of Khasi and Jayantia Hills (see Mawsynram) in the state of Meghalaya in India. * The Western Highlands of Yemen, which receive by far the most rain in Arabia. * The Western Ghats that run along India's western coast. * The Grea ...
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Snowfall
Snow comprises individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide or sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes nucleate around particles in the atmosphere by attracting supercooled water droplets, which freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns and rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow metamorphoses, by sintering, sublimation and freeze-thaw. Where the climate is co ...
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