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Cirque Mountain (Colorado)
Cirque Mountain is a mountain summit located in Ouray County of southwest Colorado, United States. It is situated six miles west of the community of Ouray, above the north side of Yankee Boy Basin, on land managed by Uncompahgre National Forest. It is part of the Sneffels Range which is a subset of the San Juan Mountains, which in turn is part of the Rocky Mountains. Cirque ranks as the 155th-highest peak in Colorado, and the ninth-highest in the Sneffels Range. It is west of the Continental Divide, 1.12 mile east of Mount Sneffels, and 0.59 mile west of Teakettle Mountain, which is the nearest higher neighbor. Topographic relief is significant as the north aspect rises above Blaine Basin in one mile, and the south aspect rises over 2,000 feet above Yankee Boy Basin in less than one mile. These basins are cirques which were carved by ancient glaciers.Ralph Lee Hopkins, Lindy Birkel Hopkins, 2000, ''Hiking Colorado's Geology'', The Mountaineers Books, , page 155. T ...
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Teakettle Mountain
Teakettle Mountain, elevation , is a summit in the Sneffels Range of southwest Colorado. The peak is west of Ouray, Colorado, Ouray in the Uncompahgre National Forest. See also *List of mountain ranges of Colorado, List of Colorado mountain ranges *List of mountains of the United States#Colorado, List of Colorado mountain summits **List of Colorado fourteeners **List of mountain peaks of Colorado#Highest major summits, List of Colorado 4000 meter prominent summits **List of the most prominent summits of Colorado *List of Colorado county high points References External links

* Mountains of Colorado Mountains of Ouray County, Colorado North American 4000 m summits {{Colorado-geo-stub ...
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Topographic Relief
Terrain or relief (also topographical relief) involves the vertical and horizontal dimensions of land surface. The term bathymetry is used to describe underwater relief, while hypsometry studies terrain relative to sea level. The Latin word (the root of ''terrain'') means "earth." In physical geography, terrain is the lay of the land. This is usually expressed in terms of the elevation, slope, and orientation of terrain features. Terrain affects surface water flow and distribution. Over a large area, it can affect weather and climate patterns. Importance The understanding of terrain is critical for many reasons: * The terrain of a region largely determines its suitability for human settlement: flatter alluvial plains tend to have better farming soils than steeper, rockier uplands. * In terms of environmental quality, agriculture, hydrology and other interdisciplinary sciences; understanding the terrain of an area assists the understanding of watershed boundaries, ...
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Mountains Of Colorado
This list includes significant mountain peaks and high points located in the United States arranged alphabetically by state, district, or territory. The highest peak or point in each state, district or territory is noted in bold. Significant mountain peaks and high points Alabama * Brindley Mountain * Cheaha Mountain, highest summit in the State of Alabama * Monte Sano Mountain *Capshaw Mountain *Dirtseller Mountain *Frog Mountain *Hawk Pride Mountain *Gunters Mountain * Sand Mountain (Alabama) *Keel Mountain (Alabama) *Halama Mountain Alaska * Afognak Mountain, summit of Afognak Island * Amak Volcano, active stratovolcano * Amherst Peak * Amulet Peak * Andy Simons Mountain * Annex Peak * Anvil Peak , active stratovolcano that forms the summit of Semisopochnoi Island * Arthur Peak * Asses Ears (Alaska) * Atna Peaks * Atuk Mountain , summit of St. Lawrence Island * Augustine Volcano, active lava dome that forms the summit of Augustine Island * Auke Mou ...
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San Juan Mountains (Colorado)
The San Juan Mountains is a high and rugged mountain range in the Rocky Mountains in southwestern Colorado and northwestern New Mexico. The area is highly mineralized (the Colorado Mineral Belt) and figured in the gold and silver mining industry of early Colorado. Major towns, all old mining camps, include Creede, Lake City, Silverton, Ouray, and Telluride. Large scale mining has ended in the region, although independent prospectors still work claims throughout the range. The last large scale mines were the Sunnyside Mine near Silverton, which operated until late in the 20th century and the Idarado Mine on Red Mountain Pass that closed down in the 1970s. Famous old San Juan mines include the Camp Bird and Smuggler Union mines, both located between Telluride and Ouray. The Summitville mine was the scene of a major environmental disaster in the 1990s when the liner of a cyanide-laced tailing pond began leaking heavily. Summitville is in the Summitville caldera, one of ...
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Mountains Of Ouray County, Colorado
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 ...
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Stony Mountain (Colorado)
Stony Mountain is a mountain summit located in Ouray County of southwest Colorado, United States. It is situated five miles southwest of the community of Ouray, on land managed by Uncompahgre National Forest. It is part of the Sneffels Range which is a subset of the San Juan Mountains, which in turn is part of the Rocky Mountains. It is situated west of the Continental Divide, 1.3 miles southwest of Potosi Peak, and 1.15 miles northeast of parent Mount Emma. Yankee Boy Basin is surrounded by Stony Mountain, Gilpin Peak, Mount Sneffels, Cirque Mountain, and Teakettle Mountain. Topographic relief is significant as the east aspect rises above Sneffels Creek in less than one mile. The mountain's name, which has been officially adopted by the United States Board on Geographic Names, was in use before 1899 when Henry Gannett published it in ''A Dictionary of Altitudes in the United States''.Henry Gannett, ''A Dictionary of Altitudes in the United States'', 1899, US Government Printi ...
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Mount Ridgway
Mount Ridgway is a mountain summit located in Ouray County of southwest Colorado, United States. It is situated five miles west of the community of Ouray, on land managed by Uncompahgre National Forest. It is part of the Sneffels Range which is a subset of the San Juan Mountains, which in turn is part of the Rocky Mountains. It is west of the Continental Divide, 2.2 miles east-northeast of Mount Sneffels, and 0.95 miles southwest of Whitehouse Mountain, which is the nearest higher neighbor. Topographic relief is significant as the west aspect rises above Blaine Basin in one mile. Etymology This mountain, the nearby town of Ridgway, the Ridgway Dam, and Ridgway State Park trace their names to Denver & Rio Grande Railroad superintendent Robert Matthew Ridgway (1834–1908), who established the town in 1891. The mountain's name has been officially adopted by the United States Board on Geographic Names. Climate According to the Köppen climate classification system, Mount R ...
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Whitehouse Mountain
Whitehouse Mountain is a mountain summit located in Ouray County, Colorado, Ouray County of southwest Colorado, United States. It is situated four miles west of the community of Ouray, Colorado, Ouray, on land managed by Uncompahgre National Forest. It is part of the Sneffels Range which is a subset of the San Juan Mountains, which in turn is part of the Rocky Mountains. It is west of the Continental Divide of the Americas, Continental Divide, 2.2 miles north of Potosi Peak, and 3.2 miles east-northeast of Mount Sneffels. Topographic relief is significant as the east aspect rises above the town of Ouray in approximately four miles. The mountain's name, which has been officially adopted by the United States Board on Geographic Names, was in use before 1906 when Henry Gannett published it in the ''Gazetteer of Colorado''.Henry Gannett, ''Gazetteer of Colorado'', 1906, US Government Printing Office, page 180. Climate According to the Köppen climate classification system, Whiteho ...
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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 ...
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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 a ...
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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'' i ...
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