Leavitt Peak
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Leavitt Peak
Leavitt Peak is located in the Emigrant Wilderness near Sonora Pass in the eastern Sierra Nevada range of California. Leavitt Peak is located on the Tuolumne County - Mono County line. The Pacific Crest Trail runs close to the east of Leavitt Peak, at an elevation of about elevation. The peak offers views south to Yosemite National Park and north towards South Lake Tahoe. Leavitt Peak is named for Hiram Leavitt, a native of New Hampshire and an early judge in Mono County. He built a hotel and home in 1863 at the foot of the east end of Sonora Pass to serve the growing number of travelers between Sonora and Aurora, primarily miners headed to the gold mines at nearby Bodie. Leavitt also erected a stagecoach station at what is called Leavitt Station. Leavitt Peak is a popular hiking destination. Leavitt Lake and Leavitt Meadow are nearby along the West Walker River and are also named for the early Leavitt family settlers. Leavitt's is recorded on Charles F. Hoffmann's map of 1873. ...
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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 ...
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Bodie, California
Bodie ( ) is a ghost town in the Bodie Hills east of the Sierra Nevada mountain range in Mono County, California, United States. It is about southeast of Lake Tahoe, and east-southeast of Bridgeport, at an elevation of 8,379 feet (2554 m). Bodie became a boom town in after the discovery of a profitable line of gold; by 1879 it had a population of 7,000–10,000. The town went into decline in the subsequent decades and came to be described as a ghost town by . The U.S. Department of the Interior recognizes the designated Bodie Historic District as a National Historic Landmark. Also registered as a California Historical Landmark, the ghost town officially was established as Bodie State Historic Park in 1962. It receives about 200,000 visitors yearly. Bodie State Historic Park is partly supported by the Bodie Foundation. History Discovery of gold Bodie began as a mining camp of little note following the discovery of gold in 1859 by a group of prospectors, including ...
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Mountains Of Tuolumne 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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Mountains Of The Sierra Nevada (United States)
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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Kennedy Lake, Kennedy Peak, And Soda Canyon From Leavitt Peak
Kennedy may refer to: People * John F. Kennedy (1917–1963), 35th president of the United States * John Kennedy (Louisiana politician), (born 1951), US Senator from Louisiana * Kennedy (surname), a family name (including a list of persons with the surname) * Kennedy (given name), a given name (including a list of person with the first name) * Kennedy (commentator) (born 1972), former MTV VJ Lisa Kennedy Montgomery, who uses "Kennedy" as a stage name * Ken Anderson (wrestler) (born 1976), American professional wrestler and actor formerly known as Mr. Kennedy Families * Kennedy family, members of which have held high political US office * Kennedy (Ireland), or O'Kennedy, a royal dynasty * Clan Kennedy, of Scotland Fictional characters * Leon S. Kennedy, a fictional character in ''Resident Evil'' * Kennedy (''Buffy the Vampire Slayer''), a fictional character in ''Buffy the Vampire Slayer'' Places Australia *Kennedy, Queensland, a locality in the Cassowary Coast Region, Q ...
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Night Cap Peak
Night Cap Peak is a 10,641-foot-elevation (3,243 meter) mountain summit located in Tuolumne County, California, United States. Description Night Cap Peak is set along the boundary of the Emigrant Wilderness on land managed by Stanislaus National Forest. The peak is part of the Sierra Nevada mountain range and is situated 2.6 miles northwest of Leavitt Peak, and three miles west-southwest of Sonora Pass. Topographic relief is significant as the summit rises over above Kennedy Meadow in three miles. Precipitation runoff from this mountain drains into Kennedy and Deadman creeks which are tributaries of the Middle Fork Stanislaus River. Etymology The peak was named "Night Cap" in the 1890s by the USGS, presumably because of its resemblance to a nightcap. The landform's present toponym was officially adopted in 1979 by the U.S. Board on Geographic Names. Climate According to the Köppen climate classification system, Night Cap Peak is located in an alpine climate zone. Mo ...
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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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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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