Mount Crocker
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Mount Crocker
Mount Crocker is a remote 12,458-foot-elevation (3,797 meter) mountain summit located on the crest of the Sierra Nevada mountain range in northern California, United States. It is situated in the John Muir Wilderness, on the boundary shared by Sierra National Forest with Inyo National Forest, and along the common border of Fresno County with Mono County. Crocker ranks as the 291st-highest summit in California. Topographic relief is significant as the north aspect rises above McGee Creek in approximately one mile. It is nine miles northeast of Lake Thomas A Edison, and approximately southeast of the community of Mammoth Lakes. History This mountain's toponym was officially adopted in 1911 by the U.S. Board on Geographic Names. The name was applied during a 1907–09 survey by Robert Bradford Marshall of the USGS to honor Charles Crocker (1822–1888), an American railroad executive who was one of the founders of the Central Pacific Railroad, which constructed the westernmost p ...
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Red And White Mountain
Red and White Mountain is a remote 12,816-foot-elevation (3,906 meter) mountain summit located on the crest of the Sierra Nevada mountain range in northern California, United States. It is situated in the John Muir Wilderness on the shared boundary of Sierra National Forest with Inyo National Forest, and along the common border of Fresno County with Mono County. It is eight miles northeast of Lake Thomas A Edison, and approximately southeast of the community of Mammoth Lakes. The nearest higher neighbor is Red Slate Mountain, to the north-northwest. History This mountain's descriptive name was applied by Theodore S. Solomons in 1894. It refers to the red slate and white granite that it is composed of. The first ascent of the summit was made July 18, 1902, by James S. Hutchinson, his brother Lincoln Hutchinson, and Charles A. Noble via the West Ridge. Norman Clyde first climbed the Northeast Ridge on July 3, 1928.R. J. Secor, ''The High Sierra Peaks, Passes, Trails'', 2009, Th ...
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Charles C Crocker By Stephen W Shaw
Charles is a masculine given name predominantly found in English and French speaking countries. It is from the French form ''Charles'' of the Proto-Germanic name (in runic alphabet) or ''*karilaz'' (in Latin alphabet), whose meaning was "free man". The Old English descendant of this word was '' Ċearl'' or ''Ċeorl'', as the name of King Cearl of Mercia, that disappeared after the Norman conquest of England. The name was notably borne by Charlemagne (Charles the Great), and was at the time Latinized as ''Karolus'' (as in ''Vita Karoli Magni''), later also as '' Carolus''. Some Germanic languages, for example Dutch and German, have retained the word in two separate senses. In the particular case of Dutch, ''Karel'' refers to the given name, whereas the noun ''kerel'' means "a bloke, fellow, man". Etymology The name's etymology is a Common Germanic noun ''*karilaz'' meaning "free man", which survives in English as churl (< Old English ''ċeorl''), which developed its depre ...
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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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Encyclopædia Britannica
The (Latin for "British Encyclopædia") is a general knowledge English-language encyclopaedia. It is published by Encyclopædia Britannica, Inc.; the company has existed since the 18th century, although it has changed ownership various times through the centuries. The encyclopaedia is maintained by about 100 full-time editors and more than 4,000 contributors. The 2010 version of the 15th edition, which spans 32 volumes and 32,640 pages, was the last printed edition. Since 2016, it has been published exclusively as an online encyclopaedia. Printed for 244 years, the ''Britannica'' was the longest running in-print encyclopaedia in the English language. It was first published between 1768 and 1771 in the Scottish capital of Edinburgh, as three volumes. The encyclopaedia grew in size: the second edition was 10 volumes, and by its fourth edition (1801–1810) it had expanded to 20 volumes. Its rising stature as a scholarly work helped recruit eminent con ...
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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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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ...
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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 Stanford (Fresno And Mono Counties, California)
Mount Stanford is a 12,838-foot-elevation (3,913 meter) mountain summit located on the crest of the Sierra Nevada mountain range in northern California, United States. It is situated in the John Muir Wilderness, on the boundary shared by Sierra National Forest with Inyo National Forest, and along the common border of Fresno County with Mono County. It is 10 miles northeast of Lake Thomas A Edison, and approximately southeast of the community of Mammoth Lakes. Topographic relief is significant as the north aspect rises above McGee Creek in approximately 1.75 mile. There is another Mount Stanford (elevation 13,979 ft) in the Sierra Nevada which is named for Stanford University. History This mountain's toponym was adopted as "Stanford Peak" in 1911 and officially revised to Mount Stanford in 1982 by the U.S. Board on Geographic Names. The name was applied during a 1907–09 survey by Robert Bradford Marshall of the USGS to honor Leland Stanford (1824–1893), the 8t ...
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Mount Huntington (California)
Mount Huntington is a mountain in the John Muir Wilderness north of Kings Canyon National Park. It is one of four peaks that surround Pioneer Basin, northwest of Mount Crocker, northeast of Mount Hopkins, and south-southwest of Mount Stanford. The mountain was named for Collis Potter Huntington, one of the builders of the Central Pacific Railroad. Climate According to the Köppen climate classification system, Mount Huntington 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 (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 cr ...), causing them to drop their moisture in the form of rain or snowfall onto the range. ...
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Mount Hopkins (California)
Mount Hopkins is a mountain in the John Muir Wilderness north of Kings Canyon National Park. It is one of four peaks that surround Pioneer Basin, south-southeast of Mount Crocker, west-southwest of Mount Huntington, and southwest of Mount Stanford. The mountain was named for Mark Hopkins, one of the builders of the Central Pacific Railroad. Climate According to the Köppen climate classification system, Mount Hopkins 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 (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 cr ...), causing them to drop their moisture in the form of rain or snowfall onto the range. Referenc ...
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The Big Four (Central Pacific Railroad)
"The Big Four" was the name popularly given to the famous and influential businessmen, philanthropists and railroad tycoons who funded the Central Pacific Railroad, (C.P.R.R.), which formed the western portion through the Sierra Nevada and the Rocky Mountains of the First Transcontinental Railroad in the United States, built from the mid-continent at the Missouri River to the Pacific Ocean during the middle and late 1860s. Composed of Leland Stanford (1824–1893), Collis Potter Huntington (1821–1900), Mark Hopkins Jr. (1813–1878), and Charles Crocker (1822–1888), the four themselves, however, personally preferred to be known as "The Associates." They enriched themselves utilizing tax money and land grants, while heavily influencing the State legislature from within the Republican party (Stanford was governor of California when the first of the Pacific Railroad Acts was passed), and through monopolizing tactics. Contemporary critics claimed they were the greatest swindler ...
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Leland Stanford
Amasa Leland Stanford (March 9, 1824June 21, 1893) was an American industrialist and politician. A member of the Republican Party, he served as the 8th governor of California from 1862 to 1863 and represented California in the United States Senate from 1885 until his death in 1893. He and his wife Jane were also the founders of Stanford University, which they named after their late son. Prior to his political career, Stanford was a successful merchant and wholesaler who built his business empire after migrating to California during the Gold Rush. As president of the Central Pacific Railroad and later the Southern Pacific from 1885 to 1890, he held tremendous power in the region and a lasting impact on California. Early life and career Leland Stanford was born in 1824 in what was then Watervliet, New York (now the Town of Colonie). He was one of eight children of Josiah and Elizabeth Phillips Stanford. Among his siblings were New York State Senator Charles Stanford (1819– ...
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