Mount Carl Heller
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Mount Carl Heller
Mount Carl Heller is a 13,211-foot-elevation (4,031 meter) mountain summit located on the crest of the Sierra Nevada mountain range in California.R. J. Secor, ''The High Sierra Peaks, Passes, Trails'', 2009, Third Edition, Mountaineers Books, , page 83. It is situated on the common border shared by Tulare County with Inyo County, as well as the shared boundary of Sequoia National Park and John Muir Wilderness. It is set west of the community of Lone Pine, north of Mount Whitney, and northwest of Tunnabora Peak, the nearest higher neighbor. Mount Carl Heller ranks as the 105th-highest summit in California. Topographic relief is significant as the west aspect rises approximately above Wallace Lake in . History The first ascent of the summit was made in August 1966 by Carl Heller and Al Green via the East Arête.John Moynier, Claude Fiddler (1993), ''Sierra Classics: 100 Best Climbs in the High Sierra'', Chockstone Press, , p. 50 This landform is unofficially named after ...
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Tunnabora Peak
Tunnabora Peak is a mountain summit located on the crest of the Sierra Nevada mountain range in California. It is situated on the common border of Tulare County with Inyo County, as well as the shared boundary of Sequoia National Park and John Muir Wilderness. It is set above the north shore of Tulainyo Lake, west of the community of Lone Pine, north-northeast of Mount Whitney, and north-northwest of Mount Carillon. Tunnabora ranks as the 51st-highest peak in California. Topographic relief is significant as it rises approximately above Whitney Portal in approximately three miles. History The first ascent of the summit was made in August 1905 by George R. Davis, USGS topographic engineer. The peak's name was submitted by the National Park Service, and officially adopted by the United States Board on Geographic Names in 1928. The etymology is uncertain, possibly Shoshonean, Mono dialect. Climate Tunnabora Peak has an alpine climate. Most weather fronts originate in the ...
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First Ascent
In mountaineering, a first ascent (abbreviated to FA in guide books) is the first successful, documented attainment of the top of a mountain or the first to follow a particular climbing route. First mountain ascents are notable because they entail genuine exploration, with greater risks, challenges and recognition than climbing a route pioneered by others. The person who performs the first ascent is called the first ascensionist. In free climbing, a first ascent (or first free ascent, abbreviated FFA) of a climbing route is the first successful, documented climb of a route without using equipment such as anchors or ropes for aiding progression or resting. History The details of the first ascents of even many prominent mountains are scanty or unknown; sometimes the only evidence of prior summiting is a cairn, artifacts, or inscriptions at the top. Today, first ascents are generally carefully recorded and usually mentioned in guidebooks. The term is also used when referrin ...
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Mount Hale (California)
Mount Hale is a mountain summit located west of the crest of the Sierra Nevada mountain range in Tulare County, California. It is situated in Sequoia National Park, 1.4 mile northwest of Mount Whitney, one mile northeast of Mount Young, and 0.85 mile west-southwest of Mount Randy Morgenson, the nearest higher neighbor. The John Muir Trail traverses below the south aspect of the mountain, providing approach access. Mt. Hale ranks as the 63rd-highest summit in California. Topographic relief is significant as the north aspect rises above Wales Lake in approximately one-quarter mile. History This mountain's name was proposed by the Sierra Club and officially adopted in 1940 by the U.S. Board on Geographic Names to honor the eminent American astronomer George Ellery Hale (1868–1938), best known for his discovery of magnetic fields in sunspots, and founder of the Mount Wilson Observatory. The immediate area has other geographical features named after astronomers, inclu ...
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Mount Randy Morgenson
Mount Randy Morgenson is a mountain summit located along the crest of the Sierra Nevada mountain range in Tulare County, California. It is situated in Sequoia National Park, one mile north-northwest of Mount Whitney, 0.85 mile east of Mount Hale, and one-half mile west of Mount Russell, the nearest higher neighbor. The John Muir Trail traverses to the south of the mountain, providing an approach option. Mt. Morgenson ranks as the 20th-highest summit in California. Topographic relief is significant as the northwest aspect rises above Wales Lake in less than one mile. History This mountain's name honors esteemed park ranger James Randall "Randy" Morgenson (1945–1996), who vanished in July 1996 while on patrol in Sequoia-Kings Canyon National Park. Despite one of the most intense search-and-rescue operations in National Park Service history, his body wasn't found until five years later. This peak's unofficial name has not been adopted by the U. S. Board on Geographic Name ...
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Trojan Peak
} Trojan Peak is a 13,947-foot-elevation (4,251 meter) mountain summit located along the crest of the Sierra Nevada mountain range in Inyo County, California. It is situated in the John Muir Wilderness, on land managed by Inyo National Forest. It is west-northwest of the community of Lone Pine, 0.7 mile (1.1 km) southeast of Mount Versteeg, and one mile (1.6 km) south-southwest of Mount Williamson, the nearest higher neighbor. Trojan Peak is rankeds as the 16th highest peak in California. Topographic relief is significant as it rises 1,427 feet (435 meters) above Lake Helen of Troy in approximately one-half mile. History The first ascent of the summit was made June 26, 1926, by Norman Clyde, who is credited with 130 first ascents, most of which were in the Sierra Nevada.{{cite web The peak's name was proposed by Chester Versteeg of the Sierra Club, and officially adopted by the United States Board on Geographic Names in 1951. As the first chairman ...
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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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Owens Valley
Owens Valley (Numic Numic is a branch of the Uto-Aztecan language family. It includes seven languages spoken by Native American peoples traditionally living in the Great Basin, Colorado River basin, Snake River basin, and southern Great Plains. The word Numic com ...: ''Payahǖǖnadǖ'', meaning "place of flowing water") is an arid valley of the Owens River in eastern California in the United States. It is located to the east of the Sierra Nevada (U.S.), Sierra Nevada, west of the White Mountains (California), White Mountains and Inyo Mountains, and north of the Mojave Desert. It sits on the west edge of the Great Basin section, Great Basin. The mountain peaks on the West side (including Mount Whitney) reach above in elevation, while the floor of the Owens Valley is about , making the valley the deepest in the United States. The Sierra Nevada casts the valley in a rain shadow, which makes Owens Valley "the Land of Little Rain." The bed of Owens Lake, now a predominantly dr ...
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Kern River
The Kern River, previously Rio de San Felipe, later La Porciuncula, is an Endangered, Wild and Scenic river in the U.S. state of California, approximately long. It drains an area of the southern Sierra Nevada mountains northeast of Bakersfield. Fed by snowmelt near Mount Whitney, the river passes through scenic canyons in the mountains and is a popular destination for whitewater rafting and kayaking. It is the southernmost major river system in the Sierra Nevada, and is the only major river in the Sierra that drains in a southerly direction. The Kern River formerly emptied into the now dry Buena Vista Lake and Kern Lake via the Kern River Slough, and Kern Lake in turn emptied into Buena Vista Lake via the Connecting Slough at the southern end of the Central Valley. Buena Vista Lake, when overflowing, first backed up into Kern Lake and then upon rising higher drained into Tulare Lake via Buena Vista Slough and a changing series of sloughs of the Kern River. The lakes wer ...
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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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Pacific Ocean
The Pacific Ocean is the largest and deepest of Earth's five oceanic divisions. It extends from the Arctic Ocean in the north to the Southern Ocean (or, depending on definition, to Antarctica) in the south, and is bounded by the continents of Asia and Oceania in the west and the Americas in the east. At in area (as defined with a southern Antarctic border), this largest division of the World Ocean—and, in turn, the hydrosphere—covers about 46% of Earth's water surface and about 32% of its total surface area, larger than Earth's entire land area combined .Pacific Ocean
. '' Britannica Concise.'' 2008: Encyclopædia Britannica, Inc.
The centers of both the

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Weather Front
A weather front is a boundary separating air masses for which several characteristics differ, such as air density, wind, temperature, and humidity. Disturbed and unstable weather due to these differences often arises along the boundary. For instance, cold fronts can bring bands of thunderstorms and cumulonimbus precipitation or be preceded by squall lines, while warm fronts are usually preceded by stratiform precipitation and fog. In summer, subtler humidity gradients are known as dry lines can trigger severe weather. Some fronts produce no precipitation and little cloudiness, although there is invariably always a wind shift. Cold fronts generally move from west to east, whereas warm fronts move poleward, although any direction is possible. Occluded fronts are a hybrid merge of the two, and stationary fronts are stalled in their motion. Cold fronts and cold occlusions move faster than warm fronts and warm occlusions because the dense air behind them can lift as well as push ...
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