Gilpin Peak
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Gilpin Peak
Gilpin Peak is a high mountain summit in the Sneffels Range of the Rocky Mountains of North America. The thirteener is located in the Mount Sneffels Wilderness of Uncompahgre National Forest, north-northeast ( bearing 23°) of the Town of Telluride, Colorado, United States, on the drainage divide between Ouray County and San Miguel County. Gilpin Peak was named in honor of William Gilpin, the first Governor of the Territory of Colorado. Climate According to the Köppen climate classification system, Gilpin Peak is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer, with a dry period in late spring. Precipitation runoff from the mountain drains into tributaries of the San Miguel and the Uncompahgre Rivers. See also * List of Colorado mountain ranges * List of Colorado mountain summits **List of Colorado fou ...
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William Gilpin (governor)
William Gilpin (October 4, 1813 – January 20, 1894) was a 19th-century US explorer, politician, land speculator, and futurist writer about the American West. He served as military officer in the United States Army during several wars, accompanied John C. Frémont on his second expedition through the West, and was instrumental in the formation of the government of the Oregon Territory. As a politician and writer, he was an inveterate believer in Manifest Destiny and was a visionary booster of new settlement to the West, helping lay the groundwork in his writings for a modern theory of the succession of civilizations. Gilpin served as the first governor of the Colorado Territory. His administration was consumed largely with the defense of the new territory in the early days of the American Civil War and was brought down after only one year by scandalous financial dealings. After the demise of his political career, he made a large fortune as a land speculator in New Mexico, alth ...
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Mount Sneffels Wilderness
The Mount Sneffels Wilderness is a wilderness area in southwest Colorado managed by the Uncompahgre National Forest. It is about west of the town of Ouray. The area is named for Mt. Sneffels, which at is a prominent fourteener in the San Juan Mountains. The word "Sneffels" is likely an Americanization of the Old Norse word for Snæfell "snow mountain," which is also the namesake of the Snæfellsnes peninsula and Snæfellsjökull Snæfellsjökull (, ''snow-fell glacier'') is a 700,000-year-old glacier-capped stratovolcano in western Iceland. It is situated on the westernmost part of the Snæfellsnes peninsula in Iceland. Sometimes it may be seen from the city of Reykjaví ... volcano in Iceland. References Wilderness areas of Colorado San Juan Mountains (Colorado) Uncompahgre National Forest Protected areas of Ouray County, Colorado Protected areas of San Miguel County, Colorado Protected areas established in 1980 1980 establishments in Colorado {{Col ...
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Gilpin Peak And Mt
Gilpin may refer to: People * Gilpin (surname), including a list of people with the surname Places United States * Gilpin, Kentucky, an unincorporated community in Casey County * Gilpin, Nevada, an unincorporated community in Storey County * Gilpin, Richmond, Virginia, a neighborhood * Gilpin County, Colorado * Gilpin Peak, a mountain in Colorado * Gilpin Township, Armstrong County, Pennsylvania Other places * River Gilpin, Cumbria, England * Gilpin, British Columbia, a community in Boundary Country, British Columbia Other uses * Gilpin Airlines, a small airline serving California, Arizona, and the Mexican states of Sonora and Baja California in the 1930s * Gilpin Baronets, a title in the Baronetage of the United Kingdom * Gilpin Homestead, Chadds Ford, Delaware County, Pennsylvania, on the US National Register of Historic Places * Gilpin Railroad, a railroad in Gilpin County from 1887 to 1917 See also * ''John Gilpin John Gilpin (18th century) was feature ...
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Uncompahgre River
The Uncompahgre River is a tributary of the Gunnison River, approximately 75 mi (121 km) long, in southwestern Colorado in the United States. Lake Como at 12,215 ft (3723m) in northern San Juan County, in the Uncompahgre National Forest in the northwestern San Juan Mountains is the headwaters of the river. It flows northwest past Ouray, Ridgway, Montrose, and Olathe and joins the Gunnison at Confluence Park in Delta. The river forms Poughkeepsie Gulch and the Uncompahgre Gorge. The major tributaries are all creeks draining the northwest San Juan Mountains. There are two dams on the Uncompahgre River, a small diversion dam in the Uncompahgre Gorge, and Ridgway Dam below the town of Ridgway which forms Ridgway Reservoir. The river is used for irrigation in the Uncompahgre Valley. Additionally, water from the Gunnison is diverted to the valley via the Gunnison Tunnel. The Uncompahgre is unnavigable except at high water. The name ''Uncompahgre'' () comes fro ...
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San Miguel River (Colorado)
The San Miguel River is a tributary of the Dolores River, approximately long, in southwestern Colorado in the United States. It rises in the San Juan Mountains southeast of Telluride and flows northwest, along the southern slope of the Uncompahgre Plateau, past the towns of Placerville and Nucla and joins the Dolores in western Montrose County approximately 15 miles (24 km) east of the state line with Utah. Geography and protected areas The San Miguel is more or less free-flowing; however, diversion dams dot the river and alter flows. In some parts it is however one of the few remaining naturally functioning rivers of the West. The San Miguel varies in gradient, from extremely steep in its upper reaches (forming a shallow, rocky, unnavigable stream) to more mellow in the lower sections ( of drop, which offers the whitewater boater a variety of runs all within the class II+--III range). All told, the San Miguel drops over from an alpine ecosystem to the desert. The ave ...
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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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Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50° to 70°N, poleward of the humid continental climates. Subarctic or boreal climates are the source regions for the cold air that affects temperate latitudes to the south in winter. These climates represent Köppen climate classification ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'', ''Dwd'' and ''Dsd''. Description This type of climate offers some of the most extreme seasonal temperature variations found on the planet: in winter, temperatures can drop to below and in summer, the temperature may exceed . However, the summers are short; no more than three months of the year (but at least one month) must have a 24-hour average temperature of at least to fall into this category of climate, and the coldest month should ave ...
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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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Gilpin Peak
Gilpin Peak is a high mountain summit in the Sneffels Range of the Rocky Mountains of North America. The thirteener is located in the Mount Sneffels Wilderness of Uncompahgre National Forest, north-northeast ( bearing 23°) of the Town of Telluride, Colorado, United States, on the drainage divide between Ouray County and San Miguel County. Gilpin Peak was named in honor of William Gilpin, the first Governor of the Territory of Colorado. Climate According to the Köppen climate classification system, Gilpin Peak is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms in summer, with a dry period in late spring. Precipitation runoff from the mountain drains into tributaries of the San Miguel and the Uncompahgre Rivers. See also * List of Colorado mountain ranges * List of Colorado mountain summits **List of Colorado fou ...
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Territory Of Colorado
The Territory of Colorado was an organized incorporated territory of the United States that existed from February 28, 1861, until August 1, 1876, when it was admitted to the Union as the State of Colorado. The territory was organized in the wake of the Pike's Peak Gold Rush of 1858–1861, which brought the first large concentration of white settlement to the region. The organic act creating the territory was passed by Congress and signed by President James Buchanan on February 28, 1861, during the secessions by Southern states that precipitated the American Civil War. The boundaries of the Colorado Territory were identical with those of the current State of Colorado. The organization of the territory helped solidify Union control over a mineral-rich area of the Rocky Mountains. Statehood was regarded as fairly imminent, but territorial ambitions for statehood were thwarted at the end of 1865 by a veto by President Andrew Johnson. Statehood for the territory was a recurring is ...
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Governor Of Colorado
The governor of Colorado is the head of government of the U.S. state of Colorado. The governor is the head of the executive branch of Colorado's state government and is charged with enforcing state laws. The governor has the power to either approve or veto bills passed by the Colorado General Assembly, to convene the legislature, and to grant pardons, except in cases of treason or impeachment. The governor is also the commander-in-chief of the state's military forces. Seven people served as governor of Colorado Territory over eight terms, appointed by the president of the United States. Since statehood, there have been 38 governors, serving 43 distinct terms. One governor Alva Adams served three non-consecutive terms, while John Long Routt, James Hamilton Peabody, and Edwin C. Johnson each served during two non-consecutive periods. The longest-serving governors were Richard "Dick" Lamm (1975–1987) and Roy Romer (1987–1999), who each served 12 years over three terms. The ...
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Drainage Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it is ...
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