Thatchtop
Thatchtop is a mountain summit in Larimer County, Colorado, United States. Description Thatchtop is set one mile east of the Continental Divide in the Front Range of the Rocky Mountains. The mountain is situated within Rocky Mountain National Park, approximately southwest of Estes Park. Precipitation runoff from the mountain drains into tributaries of Glacier Creek which in turn is a tributary of the Big Thompson River. Topographic relief is significant with the summit rising above Glacier Gorge in 0.75 mile (1.21 km). Etymology The mountain's descriptive name refers to the matted groundcover of the roof-shaped mountain. The landforms's toponym was officially adopted in 1932 by the United States Board on Geographic Names, although it appeared in publications as early as 1911 if not earlier. The Arapaho called the mountain "Buffalo Climb."Randi Minetor (2019), ''Historic Rocky Mountain National Park'', Lyons Press, , p. 21. Climate According to the Köppen clima ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Otis Peak
Otis Peak is a mountain summit on the boundary shared by Grand County and Larimer County, in Colorado, United States. Description Otis Peak is set along the Continental Divide in the Front Range of the Rocky Mountains. The mountain is situated within Rocky Mountain National Park and southwest of Estes Park. Precipitation runoff from the mountain drains chiefly into tributaries of Glacier Creek which in turn is a tributary of the Big Thompson River, and the lower west slope drains to Grand Lake via North Inlet. A portion of that water that arrives at Grand Lake is then diverted to the east side of the Continental Divide via the Alva B. Adams Tunnel which is bored under Otis Peak. Topographic relief is significant as the summit rises above Loch Vale in one mile. Etymology The mountain's toponym was reported in publications as early as 1915, and was officially adopted in 1932 by the United States Board on Geographic Names. The peak is named for Dr. Edward Osgood Otis (1848� ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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The Sharkstooth
The Sharkstooth is a mountain summit in Larimer County, Colorado, United States. Description The Sharkstooth is set 1,500 feet east of the Continental Divide in the Front Range of the Rocky Mountains. It is in the "Cathedral Spires" area, and is the second-steepest point in Colorado. The summit is situated within Rocky Mountain National Park, approximately southwest of Estes Park. Precipitation runoff from the mountain drains into tributaries of Glacier Creek which in turn is a tributary of the Big Thompson River. Topographic relief is significant with the summit rising above Loch Vale in one mile. The landforms's toponym has been officially adopted by the United States Board on Geographic Names. Climate According to the Köppen climate classification system, The Sharkstooth is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers. Due to its altitude, it receives precipitation all year, as snow in winter, and as thunderstorms ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Powell Peak
Powell Peak is a summit in Grand County, Colorado, in the United States. With an elevation of , Powell Peak is the 493rd-highest summit in the state of Colorado. The peak was named for John Wesley Powell. The mountain's toponym was officially adopted in 1961 by the United States Board on Geographic Names. Precipitation runoff from the mountain's east slope drains into Glacier Creek which is a tributary of the Big Thompson River, and the west slope drains to Grand Lake via North Inlet. Climate According to the Köppen climate classification system, the peak is located in an alpine subarctic climate zone with 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. See also * List of peaks in Rocky Mountain National Park The list of peaks in Rocky Mountain National Park includes the following: References {{Rocky Mountain National Park ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Big Thompson River
The Big Thompson River is a tributary of the South Platte River, approximately 78 miles (123 km) long, in the U.S. state of Colorado. Originating in Forest Canyon in Rocky Mountain National Park, the river flows into Lake Estes in the town of Estes Park and then through Big Thompson Canyon. It includes four crossings/bridges which are listed on the U.S. National Register of Historic Places. Course of the river The headwaters of the Big Thompson River begin in Forest Canyon within Rocky Mountain National Park in Larimer County, Colorado. The river flows east through Moraine Park to the town of Estes Park. There it is held in Lake Estes by Olympus Dam before being released into the Big Thompson Canyon. The North Fork Big Thompson River also begins in Rocky Mountain National Park, on the northern slopes of the Mummy Range. This tributary flows east, through the town of Glen Haven, where it merges with the Big Thompson River in the town of Drake, in the Big Thomps ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mountains Of Rocky Mountain National Park
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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mountains Of Larimer 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 terrain and ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Taylor Peak (Grand County, Colorado)
Taylor Peak, elevation , is a summit in the Front Range of north central Colorado. The peak is in Rocky Mountain National Park Rocky Mountain National Park is an American national park located approximately northwest of Denver in north-central Colorado, within the Front Range of the Rocky Mountains. The park is situated between the towns of Estes Park to the east and ... at the head of Loch Vale and just north of Taylor Glacier. Historical names *Taylor Peak – 1932 *The Bangs See also * List of Colorado mountain ranges * List of Colorado mountain summits ** List of Colorado fourteeners ** 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 Rocky Mountain National Park Mountains of Grand County, Colorado Mountains of Larimer County, Colorado North American 4000 m summits {{Colorado-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Longs Peak
Longs Peak ( Arapaho: ) is a high and prominent mountain in the northern Front Range of the Rocky Mountains of North America. The fourteener is located in the Rocky Mountain National Park Wilderness, southwest by south ( bearing 209°) of the Town of Estes Park, Colorado, United States. Longs Peak is the northernmost fourteener in the Rocky Mountains of Colorado and the highest point in Boulder County and Rocky Mountain National Park. The mountain was named in honor of explorer Stephen Harriman Long and is featured on the Colorado state quarter.The elevation of Longs Peak includes an adjustment of +1.652 m (+5.42 ft) from NGVD 29 to NAVD 88. Description Longs Peak can be prominently seen from Longmont, Colorado, as well as from most of the northern Front Range Urban Corridor. It is one of the most prominent mountains in Colorado, rising above the western edge of the Great Plains. The peak is named for Major Stephen Harriman Long, who is sai ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Arapaho
The Arapaho (; french: Arapahos, ) are a Native American people historically living on the plains of Colorado and Wyoming. They were close allies of the Cheyenne tribe and loosely aligned with the Lakota and Dakota. By the 1850s, Arapaho bands formed two tribes, namely the Northern Arapaho and Southern Arapaho. Since 1878, the Northern Arapaho have lived with the Eastern Shoshone on the Wind River Reservation in Wyoming and are federally recognized as the Arapahoe Tribe of the Wind River Reservation. The Southern Arapaho live with the Southern Cheyenne in Oklahoma. Together, their members are enrolled as the federally recognized Cheyenne and Arapaho Tribes. Names It is uncertain where the word 'Arapaho' came from. Europeans may have derived it from the Pawnee word for "trader", ''iriiraraapuhu'', or it may have been a corruption of a Crow word for "tattoo", ''alapúuxaache''. The Arapaho autonym is or ("our people" or "people of our own kind"). They refer to the ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |