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Cardinal Mountain
Cardinal Mountain is a 13,396-foot-elevation (4,083 meter) mountain summit located on the crest of the Sierra Nevada mountain range in northern California. It is situated on the common border of Fresno County with Inyo County, as well as the shared boundary of John Muir Wilderness and Kings Canyon National Park. It is south-southwest of the community of Big Pine, approximately one mile north of Taboose Pass, and one mile south-southeast of Split Mountain, which is the nearest higher neighbor. Cardinal Mountain ranks as the 73rd highest summit in California. The first ascent of the summit was made August 11, 1922, by George Downing, Jr. The standard approach is via the Taboose Pass Trail, and the John Muir Trail passes west of this peak, providing an approach option to the mountain. The mountain's descriptive name was given by George R. Davis, a USGS topographer, on account of the brilliant red color of the roof pendant, like the red cap of a cardinal. Climate According to the Kö ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cardinal (color)
Cardinal is a vivid red, which may get its name from the cassocks worn by Catholic cardinals (although the color worn by cardinals is scarlet). The cardinal bird also takes its name from the cardinal bishops. The first recorded use of ''cardinal'' as a color name in English was in the year 1698. Maerz and Paul ''A Dictionary of Color'' New York:1930 McGraw-Hill Page 192; Color Sample of Cardinal: Page 33 Plate 5 Color Sample L5 Cardinal in other color systems The corresponding Pantone Matching System (PMS) color is 200, as seen in the school colors for Wisconsin, Arizona and Wesleyan, and as one of the two official colors of the Phi Kappa Psi and Alpha Sigma Phi Fraternities and the only official color of the sorority Alpha Omicron Pi. However, Stanford's, M.I.T.´s, and USC´s PMS color is 201, while Carnegie Mellon and Worcester Polytechnic Institute use PMS 187, Brown University uses PMS 192, Iowa State University uses PMS 186, and Ball State University uses P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roof Pendant
In structural geology, a roof pendant, also known as a pendant, is a mass of country rock that projects downward into and is entirely surrounded by an igneous intrusion such as a batholith or other pluton. In lay terminology sometimes "rock hat" is used. A roof pendant is an erosional remnant that was created by the removal of the overlying country rock that formed the roof of the igneous intrusion that encloses it. If this downward protruding mass of roof rock still has a connection to the main, surrounding mass of country rock, they are known by structural geologists as either ''septa'' or ''screens.''U.S. Bureau of Mines Staff (1996) ''Dictionary of Mining, Mineral, & Related Terms.'' Report SP-96-1, U.S. Department of Interior, U.S. Bureau of Mines, Washington, D.C.Neuendorf, KKE, JP Mehl, Jr., and JA Jackson, eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Best, MG (2003) ''Igneous and metamorphic petrology, 2nd ed.'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Kings Canyon National Park
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 (topography), 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, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Tinemaha
Mount Tinemaha is a mountain summit located east of the crest of the Sierra Nevada mountain range, in Inyo County of northern California. It is situated on the eastern boundary of the John Muir Wilderness, on land managed by Inyo National Forest. It is 1.3 mile southeast of Tinemaha Lake, and 1.8 mile northeast of parent Split Mountain. Topographic relief is significant as the east aspect rises above Owens Valley in two miles. History This mountain's name was officially adopted in 1937 by the U.S. Board on Geographic Names to honor the legendary Paiute chief, Tinemaha. The peak was known by this name to the early prospectors and cattlemen of Owens Valley. The first ascent of the summit was made July 1, 1937, by Chester Versteeg, a prominent Sierra Club member. Chester Versteeg submitted the name to the board for consideration. Climate According to the Köppen climate classification system, Mount Tinemaha has an alpine climate. Most weather fronts originate in the Pacific Ocean, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountain Peaks Of California
This article comprises three sortable tables of Summit, 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 peak, ultra-prominent summit is a summit with at least of topographic prominence. of the United States, U.S. California, State of California. The summit of a mountain or hill may be measured in three principal ways: #The Elevation, topographic elevation of a summit measures the height of the summit above a Geoid, 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 Survey]noteIf the elevation or prominence of a summit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Owens Valley
Owens Valley (Numic: ''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, west of the White Mountains and Inyo Mountains, and north of the Mojave Desert. It sits on the west edge of the 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 dry endorheic alkali flat, sits on the southern end of the valley. The valley provides water to the Los Angeles Aqueduct, the source of one-third of the water for Los Angeles, and was the area at the center of one of the fiercest and longest-running episodes of the California Water Wars. These episodes inspired aspects of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Fork Kings River
The South Fork Kings River is a tributary of the Kings River in the Sierra Nevada of Fresno County, California. The river forms part of Kings Canyon, the namesake of Kings Canyon National Park and one of the deepest canyons in North America with a maximum relief of from rim to river. Course The South Fork is the largest headwater of the Kings River. It originates at an elevation of at an unnamed lake in Kings Canyon National Park, south of Mather Pass and west of Split Mountain, in a high alpine basin known as Upper Basin. It flows south, and is paralleled for several miles by the combined Pacific Crest Trail/ John Muir Trail. The trail and river separate at a point west of Taboose Pass, where the river turns to the southwest through a deep gorge between Cirque Crest to the northwest and Arrow Ridge to the southeast. To the east, the Muro Blanco cliffs rise more than half a mile (0.8 km) above the river. The river flows into Paradise Valley, where it flows in a south-s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 we ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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