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Mount Rose (Nevada)
Mount Rose is the highest mountain in Washoe County, within the Carson Range of Nevada, United States. It ranks thirty-seventh among the most topographically prominent peaks in the state. It is also both the highest and most topographically prominent peak of the greater Sierra Nevada range within the state of Nevada, and the third most topographically prominent peak in the Sierra Nevada overall. It is located in the Mount Rose Wilderness of the Humboldt-Toiyabe National Forest. An extinct volcano, the mountain is in between Lake Tahoe and Reno. State Route 431 traverses Mount Rose Summit southeast of Mount Rose. Due to the high elevation, most of the precipitation that falls on the mountain is snow. The view from Mount Rose, facing east is the Truckee Meadows area is the second largest population center in Nevada. According to one tradition, the peak was named after Jacob S, Rose, an early settler, while another tradition states the mountain has the name of Rose Hickman ...
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Carson Range
The Carson Range is a spur of the Sierra Nevada in eastern California and western Nevada that starts at Carson Pass and stretches north to the Truckee River near Verdi, Nevada. Geography The mountain range is about 50 miles (80 km) long and 5–10 miles (8–16 km) wide, with 3/4 of the range lying within the state of Nevada. The Carson Range, along with its parent the Sierra Nevada, together cast a rain shadow over the Greater Reno Area and Carson City. Unlike the main crest of the Sierra Nevada to the west of Lake Tahoe, the Carson Range loses its snow much earlier (April), and gains it much later (December). In fact, it receives about half the snowfall as mountains west of the lake. Meltwater from the range feeds into the Truckee River and West Fork Carson River, as well as Lake Tahoe and Marlette Lake. ;Principal Mountains Transportation The western slopes of the range form the eastern shoreline of Lake Tahoe, along which US 50 and NV 28 form a partial ring r ...
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Google
Google LLC () is an American multinational technology company focusing on search engine technology, online advertising, cloud computing, computer software, quantum computing, e-commerce, artificial intelligence, and consumer electronics. It has been referred to as "the most powerful company in the world" and one of the world's most valuable brands due to its market dominance, data collection, and technological advantages in the area of artificial intelligence. Its parent company Alphabet is considered one of the Big Five American information technology companies, alongside Amazon, Apple, Meta, and Microsoft. Google was founded on September 4, 1998, by Larry Page and Sergey Brin while they were PhD students at Stanford University in California. Together they own about 14% of its publicly listed shares and control 56% of its stockholder voting power through super-voting stock. The company went public via an initial public offering (IPO) in 2004. In 2015, Google was reor ...
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Mountains Of Washoe County, Nevada
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 ...
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Desert Climate
The desert climate or arid climate (in the Köppen climate classification ''BWh'' and ''BWk''), is a dry climate sub-type in which there is a severe excess of evaporation over precipitation. The typically bald, rocky, or sandy surfaces in desert climates are dry and hold little moisture, quickly evaporating the already little rainfall they receive. Covering 14.2% of earth's land area, hot deserts are the second most common type of climate on earth after the polar climate. There are two variations of a desert climate according to the Köppen climate classification: a hot desert climate (''BWh''), and a cold desert climate (''BWk''). To delineate "hot desert climates" from "cold desert climates", there are three widely used isotherms: most commonly a mean annual temperature of , or sometimes the coldest month's mean temperature of , so that a location with a ''BW'' type climate with the appropriate temperature above whichever isotherm is being used is classified as "hot arid sub ...
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Hot Semi-arid Climate
A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes. Defining attributes of semi-arid climates A more precise definition is given by the Köppen climate classification, which treats steppe climates (''BSk'' and ''BSh'') as intermediates between desert climates (BW) and humid climates (A, C, D) in ecological characteristics and agricultural potential. Semi-arid climates tend to support short, thorny or scrubby vegetation and are usually dominated by either grasses or shrubs as it usually can't support forests. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. The method used to find the precipitation threshold (in millimeters): *multiply by ...
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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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Humid Continental Climate
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers and freezing cold (sometimes severely cold in the northern areas) winters. Precipitation is usually distributed throughout the year but often do have dry seasons. The definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below or depending on the isotherm, and there must be at least four months whose mean temperatures are at or above . In addition, the location in question must not be semi-arid or arid. The cooler ''Dfb'', ''Dwb'', and ''Dsb'' subtypes are also known as hemiboreal climates. Humid continental climates are generally found between latitudes 30° N and 60° N, within the central and northeastern portions of North America, Europe, and Asia. They are rare and isolat ...
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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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Three-thousander
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Andes) ...
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Mount Rose Weather Observatory
The Mount Rose Weather Observatory was established on June 29, 1905, on the summit, making it one of the oldest high altitude weather observatories in the United States. Dr. James Edward Church established the observatory and established a snow survey system to measure the amount of water contained in the snow pack. The observatory featured many design features that were unique or revolutionary for its time. This included the ability to record data without anyone at the site. The building was built to be able to shed accumulated snow from the roof without manual assistance. The observatory was a department of the University of Nevada. The site is marked as Nevada Historical Marker Nevada historical markers identify significant places of interest in Nevada's history. The Historic Marker Program was initiated by the Nevada State Legislature in 1967 to bring the state's heritage to the public's attention with on-site markers. ... 230. References {{coord missing, Nevada ...
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James E
James is a common English language surname and given name: *James (name), the typically masculine first name James * James (surname), various people with the last name James James or James City may also refer to: People * King James (other), various kings named James * Saint James (other) * James (musician) * James, brother of Jesus Places Canada * James Bay, a large body of water * James, Ontario United Kingdom * James College, a college of the University of York United States * James, Georgia, an unincorporated community * James, Iowa, an unincorporated community * James City, North Carolina * James City County, Virginia ** James City (Virginia Company) ** James City Shire * James City, Pennsylvania * St. James City, Florida Arts, entertainment, and media * ''James'' (2005 film), a Bollywood film * ''James'' (2008 film), an Irish short film * ''James'' (2022 film), an Indian Kannada-language film * James the Red Engine, a character in ''Thomas the Tank En ...
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Slide Mountain (Nevada)
Slide Mountain is a peak in the Carson Range near Reno, in Washoe County, Nevada. From the summit of Slide Mountain, Lake Tahoe, Washoe Lake, Carson Valley, and the city of Reno can be viewed. History Slide Mountain is named after the repeated large landslides that occur high on the mountain's south east side. The slide areas are devoid of trees and vegetation and are covered in granite rock and decomposed granite sand. This gives the barren slopes a whitish color, and the distinctive slide zones are plainly visible from points to the southeast of the mountain in Washoe Valley. The most recent large slide occurred on May 30, 1983. The slide ran immediately into Price Lake in a small valley halfway down the mountain. The resulting slurry of granite sand, granite rock, and forest debris flowed freely down the canyon below Price Lake, and ran out on the flat floor of Washoe Valley. The debris flow severed the older US 395 highway, and partially covered the newer US 395 freeway. ...
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