Mount Goode (California)
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Mount Goode (California)
Mount Goode is a 13,085-foot-elevation (3,988 meter) mountain summit located on the crest of the Sierra Nevada mountain range in California, United States. It is situated on the shared boundary of Kings Canyon National Park with John Muir Wilderness, and along the common border of Fresno County with Inyo County. It is also approximately one mile west-northwest of Bishop Pass, one mile east-southeast of Mount Johnson, south of Hurd Peak, and west of the community of Big Pine. History This mountain's name and location were officially adopted in 1926 by the U.S. Board on Geographic Names based on a recommendation by the Sierra Club. Prior to 1926, the USGS placed Mount Goode at the location of Black Giant. The name commemorates Richard Urquhart Goode (1858–1903), geographer for the United States Geological Survey, in charge of the Pacific Division, Topographic Branch. The first ascent of the peak was made July 16, 1939, by Chester Versteeg, a prominent Sierra Club member. Cl ...
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Mount Gilbert (California)
Mount Gilbert is a mountain located on the crest of the Sierra Nevada range in California, United States. It is situated on the shared boundary of Kings Canyon National Park and John Muir Wilderness, and along the common border of Fresno County, California, Fresno County and Inyo County, California, Inyo County. It is west of the community of Big Pine, California, Big Pine, 0.8 mile (1.3 km) northwest of Mount Johnson (California), Mount Johnson, and one mile (1.6 km) southeast of Mount Thompson, which is its nearest higher neighbor. Mount Gilbert ranks as the 127th-highest summit in California. Topographic relief is significant as the south aspect rises above LeConte Canyon in less than two miles, and the northern aspect rises 3,340 feet above South Lake in 2.5 miles. History This mountain's name commemorates eminent geologist Grove Karl Gilbert (1843–1918), who worked much of the Sierra Nevada range with the Wheeler Survey. The mountain's name was officially adopted i ...
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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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Goode Mountain
Goode Mountain is one of the major peaks of the North Cascades in the U.S. state of Washington. Named for topographer Richard U. Goode of the USGS, it is the highest peak located in North Cascades National Park, between the Skagit River and Lake Chelan. It is the fourth-highest non-volcanic peak in Washington, and the twelfth-highest summit overall. Goode Mountain is a massive mountain, rising over from its footings, and almost from the bottom of Bridge creek valley. The mountain is made up of one main peak, and two smaller sub-peaks, The West Tower, and southeast peak. Both are over . On the northeast side it accomplishes this rise in only 1.6 horizontal miles (2.6 km). However, due to its isolated location in the rugged North Cascades, it is not visible from any major road. Goode Glacier is also located on the northeast slopes of the mountain, in addition to many small snowfields located at higher elevations. Other major features of the mountain are Greenview Lake e ...
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Mount Goode
Mount Goode, pronounced like "good", is a prominent glaciated mountain summit located in the Chugach Mountains, in the U.S. state of Alaska. The peak is situated east of Anchorage, northwest of College Fjord, west of Mount Grace, and southwest of Mount Marcus Baker, on land managed  by Chugach National Forest. History This mountain is called ''Skitnu Dghelaya'', meaning Brush River Mountain, in the Denaʼina language. The Mount Goode name was officially adopted March 5, 1924, by the U.S. Board on Geographic Names to commemorate Richard Urquhart Goode (1858-1903), geographer for the United States Geological Survey, in charge of the Pacific Division, Topographic Branch, at the time when work in the Alaska area was first conducted. The first ascent of the peak was made in April 1966 by John Vincent Hoeman and Helmut Tschaffert.Michael Wood and Colby Holmes, ''Alaska: A Climbing Guide'', The Mountaineers Books, 2001, page 132.  Climate Based on the Köppen climate classifica ...
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Bishop Creek (Inyo County)
:''Bishop Creek is also a dated variant of Baxter Creek in Richmond/El Cerrito, California'' Bishop Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed March 17, 2011 stream in Inyo County, California. It is the largest tributary of the Owens River. It has five hydroelectric plants owned by Southern California Edison, Bishop Creek #2–6. Bishop Creek #1 was never completed. Parts of the creek run through pipelines, or penstocks, to increase output at the power plants. Bishop Creek has three forks, North, Middle and South. All have their headwaters in the eastern Sierra Nevada, near the border with Fresno County. The forks all flow into lakes while still at high elevations. The North Fork flows into North Lake, the Middle Fork flows into Lake Sabrina. The North and Middle forks combine above and flow through the community of Aspendell and below it the combined creeks are dammed at Intake Two, a reservoir. The Sou ...
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Owens River
The Owens River is a river in eastern California in the United States, approximately long.U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed March 17, 2011, It drains into and through the Owens Valley, an arid basin between the eastern slope of the Sierra Nevada and the western faces of the Inyo and White Mountains. The river terminates at the endorheic Owens Lake south of Lone Pine, at the bottom of a watershed. In the early 1900s, the Owens River was the focus of the California Water Wars, fought between the city of Los Angeles and the inhabitants of Owens Valley over the construction of the Los Angeles Aqueduct. Since 1913, the Owens River has been diverted to Los Angeles, causing the ruin of the valley's economy and the drying of Owens Lake. In winter 2006, the Los Angeles Department of Water and Power restored 5% of the pre-aqueduct flow to the river by court order, allowing the Owens River Gorge, the river bed in ...
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Kings River (California)
The Kings River is a river draining the Sierra Nevada (U.S.), Sierra Nevada mountain range in central California in the United States. Its headwaters originate along the Sierra Crest in and around Kings Canyon National Park and form the eponymous Kings Canyon, one of the deepest river gorges in North America. The river is impounded in Pine Flat Lake before flowing into the San Joaquin Valley (the southern half of the Central Valley (California), Central Valley) southeast of Fresno, California, Fresno. With its upper and middle course in Fresno County, California, Fresno County, the Kings River diverges into multiple branches in Kings County, California, Kings County, with some water flowing south to the old Tulare Lake bed and the rest flowing north to the San Joaquin River. However, most of the water is consumed for irrigation well upstream of either point. Inhabited for thousands of years by the Yokuts people, Yokuts and other native groups, the Kings River basin once fed a va ...
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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 ...
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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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Snowfall
Snow comprises individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide or sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes nucleate around particles in the atmosphere by attracting supercooled water droplets, which freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns and rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow metamorphoses, by sintering, sublimation and freeze-thaw. Where the climate is co ...
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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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