|
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sierra Peaks Section
The Sierra Peaks Section (SPS) is a mountaineering society within the Angeles Chapter of the Sierra Club that serves to provide mountaineering activities for Sierra Club members in the Sierra Nevada, and to honor mountaineers who have summited Sierra Nevada peaks. History The Sierra Peaks Section was established in 1955. The Section maintains historic summit registers at Bancroft Library on the University of California, Berkeley campus. Membership To become a member of the SPS, one must be a Sierra Club member and have climbed at least six peaks on the SPS List; it is not necessary that the peaks be Emblem peaks. For verification purposes, two of those ascents must be done on an official SPS trip. Especially accomplished members are award with ''emblems'', with the following grades (from highest to lowest): * Third List Completion * Second List Completion * First List Completion * Master Emblem * Senior Emblem * Emblem Upon receiving one of the normal emblems, members may be re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Stanford
Mount Stanford, at an elevation of , is on the Kings-Kern Divide in Kings Canyon National Park. It is named for Stanford University. It is the fifteenth tallest mountain in California and is located about from University Peak (California), University Peak which was named for the University of California. History On August 1, 1896 Professor Bolton Brown, Bolton Coit Brown of Stanford made the first recorded ascent and requested that it be named Mount Stanford. Since there was another peak with the same name in Placer County, California, Placer County, he suggested the peak he climbed be named Stanford University peak if his first choice was rejected. The decision was made to give the name Castle Peak (California), Castle Peak to the summit in Placer County and Brown's first choice was accepted. Three years later, on August 16, 1899, Stanford University's President, David Starr Jordan, also make the ascent with his wife and a party from Stanford. He had previously climbed in 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 well as push ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charles Crocker
Charles Crocker (September 16, 1822 – August 14, 1888) was an American railroad executive who was one of the founders of the Central Pacific Railroad, which constructed the westernmost portion of the first transcontinental railroad, and took control with partners of the Southern Pacific Railroad. Early years Crocker was born in Troy, New York on September 16, 1822. He was the son of Eliza (née Wright) and Isaac Crocker, a modest family. They joined the nineteenth-century migration west and moved to Indiana when he was 14, where they had a farm. Crocker soon became independent, working on several farms, a sawmill, and at an iron forge. At the age of 23, in 1845, he founded a small, independent iron forge of his own. He used money saved from his earnings to invest later in the new railroad business after moving to California, which had become a boom state since the Gold Rush. His older brother Edwin B. Crocker had become an attorney by the time Crocker was investing in rail ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_-_11.jpg "Click for more on -> First Ascent")
