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Lulu Mountain
Lulu Mountain is a summit in Colorado, United States. Description Lulu Mountain is situated on the Continental Divide of the Americas, Continental Divide along the boundary shared by Grand County, Colorado, Grand County and Jackson County, Colorado, Jackson County. It is the 20th-highest peak of the Never Summer Mountains which are a subrange of the Rocky Mountains. The mountain is situated on the boundary that Rocky Mountain National Park shares with Medicine Bow–Routt National Forest. Precipitation runoff from the mountain's north slope drains into the headwaters of the Michigan River, whereas the south slope drains into headwaters of the Colorado River except for a portion which is diverted by the Grand Ditch. Topographic relief is significant as the summit rises above the Colorado River in and above the Michigan River in one-half mile (0.8 km). Climate According to the Köppen climate classification system, Lulu Mountain is located in an alpine subarctic climate zon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Richthofen
Mount Richthofen is the highest summit of the Never Summer Mountains range of the Rocky Mountains of North America. The prominent peak is located northwest by west ( bearing 308°) of Milner Pass, Colorado, United States, on the Continental Divide separating the Rocky Mountain National Park Wilderness in Rocky Mountain National Park and Grand County from Routt National Forest and Jackson County. The mountain was named in honor of pioneering German geologist Baron Ferdinand von Richthofen, apparently by Clarence King's 1870 survey team. Mountain Needles and Grenadiers explorer William S. Cooper climbed Mount Richthofen by himself in 1908 in what is presumed to be the first ascent in historic times by Americans of European descent. No sign of previous climbers were present at that time. Today, the mountain is typically climbed from Lake Agnes to the north, easily reachable from Cameron Pass. The mountain is a steep Class 3 climb that often requires travel on steep scree s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Mountains Of Jackson 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. 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, ecosystems of mountains: different el ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Grand 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nokhu Crags
Nokhu Crags is a rock formation and mountain summit in the Never Summer Mountains range of the Rocky Mountains of North America. The name is derived from the Arapaho language, ''Neaha-no-xhu'', meaning "Eagles Nest." The peak is located in State Forest State Park, south ( bearing 181°) of Cameron Pass in Jackson County, Colorado, United States. The summit lies just northwest of the Continental Divide and Rocky Mountain National Park, near the headwaters of the Michigan River. The peak is prominently visible from State Highway 14 and can be seen throughout the southern North Park basin where it is known also known as "the Crags" or "Sleeping Indian" for its resemblance to the form of a supine chief. To the east lie the shallow basins of Snow Lake and the Michigan or American Lakes; to the north lies a snow filled couloir; to the west the mountain descends directly into the deep waters of Lake Agnes; and to the south lie Static Peak, Mount Richthofen, and the remainder o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Static Peak (Colorado)
Static Peak is a mountain peak in the U.S. state of Colorado, within State Forest State Park and part of the Never Summer Mountain Range. It is located in a chain of peaks and lies between Nokhu Crags to the north and Mount Richthofen to the south. To the east lie the shallow basins of Snow Lake and to the west the mountain descends directly into the deep waters of Lake Agnes. Geology Approximately 24–29 million years ago, rising magma began to create volcanoes that were the predecessors of the Never Summer Mountains. The magma cooled into granitic formations that have weathered into the current mountain range. 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 This is a list of all 64 counties of the U.S. State of Colorado by their points of highest elevation. Of the 50 hig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kawuneeche Valley
Kawuneeche Valley, also known as Kawuneeche or Coyote Valley, is a marshy valley of the Colorado River near its beginning. It is located on the west side of Rocky Mountain National Park in Colorado. The axis of the valley runs almost directly north to south. Kawuneeche means "valley of the coyote" in Arapaho language and there is a Coyote Valley Trail head by US Route 34 in the western half of the park. Coyotes still live here, as do wapiti (elk), mule deer, moose (reintroduced in 1978 into nearby North Park), and mountain lion. Along the main part of valley runs the lower section of the Trail Ridge Road - the highest continuous paved road in the United States. Wilderness The construction of a water diversion canal called Grand Ditch between the 1890s and 1930s reduced the water table and limited the frequency and magnitude of the floods in the Kawuneeche Valley. Grand Ditch collects water from Colorado River’s tributaries in the Never Summer Mountains like a rain gutter ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
La Poudre Pass
La Poudre Pass (elevation ), a high mountain pass, is located in the Rocky Mountains of northern Colorado in the United States. The pass straddles the Continental Divide, and separates the headwaters of La Poudre Pass Creek, which joins the Cache la Poudre River and eventually empties into the Gulf of Mexico, from the headwaters of the Colorado River, which drains into the Gulf of California. At the pass, the Continental Divide is the boundary between Grand and Larimer counties, and is also the northern boundary of Rocky Mountain National Park. The pass itself is a broad, flat, swampy area. In the wet meadow just south of the divide, the Colorado River begins its course as a tiny stream emerging from this area which included the small La Poudre Pass Lake. The Rocky Mountain National Park La Poudre Pass Ranger Station is also located in the pass.''Fall River Pass, Colorado,'' 7.5 Minute Topographic Quadrangle, USGS, 1958 (1985 rev.) The pass is traversed by a hiking trail, by ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States Board On Geographic Names
The United States Board on Geographic Names (BGN) is a federal body operating under the United States Secretary of the Interior. The purpose of the board is to establish and maintain uniform usage of geographic names throughout the federal government of the United States. History On January 8, 1890, Thomas Corwin Mendenhall, superintendent of the US Coast and Geodetic Survey Office, wrote to 10 noted geographers "to suggest the organization of a Board made up of representatives from the different Government services interested, to which may be referred any disputed question of geographical orthography." President Benjamin Harrison signed executive order 28 on September 4, 1890, establishing the ''Board on Geographical Names''. "To this Board shall be referred all unsettled questions concerning geographic names. The decisions of the Board are to be accepted y federal departmentsas the standard authority for such matters." The board was given authority to resolve all unsettled q ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lulu City, Colorado
Lulu City was a transient mining town in eastern Grand County, Colorado, in the Kawuneeche Valley in what is now Rocky Mountain National Park. The town appeared after silver was discovered in the area in 1879 by prospector Joe Shipler, and was built primarily by the Middle Park and Grand River Land Improvement Company in 1880. The company was backed by Benjamin F. Burnett of Fort Collins and Fort Collins rancher William Baker. The town was named after Burnett's daughter. By 1881, there were forty cabins and a number of business establishments. By this time it was apparent that the silver ore was of low grade, and that high transportation costs made mining in the area marginal, and the town began its decline. It was abandoned by 1885, except by Shipler, who lived there for thirty years. The settlement of Dutchtown was established in the Never Summer Mountains to the west of town by outcasts from Lulu City. The land was purchased from the estate of Hugh J. Harrison by the Nationa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
