Mount Stratus
   HOME
*





Mount Stratus
Mount Stratus is a mountain summit in Grand County, Colorado, United States. Description Mount Stratus is the ninth-highest peak of the Never Summer Mountains which are a subrange of the Rocky Mountains. The mountain is situated on the western boundary of Rocky Mountain National Park and is visible from Trail Ridge Road within the park. The west side of the peak is in the Never Summer Wilderness which is managed by Arapaho National Forest. Precipitation runoff from the mountain's slopes drains into tributaries 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 Kawuneeche Valley in and above Baker Gulch in three-quarters of a mile. An ascent of the peak involves hiking round-trip with of elevation gain. Etymology The mountain's toponym has been officially adopted by the United States Board on Geographic Names. In 1914, James Grafton Rogers named Mount Cirrus, Mount Nimbus, ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Mount Nimbus
Mount Nimbus is a mountain summit in Grand County, Colorado, Grand County, Colorado, United States. Description Mount Nimbus is set along the Continental Divide of the Americas, Continental Divide and is the fifth-highest peak of the Never Summer Mountains which are a subrange of the Rocky Mountains. The mountain is situated on the western boundary of Rocky Mountain National Park and is visible from Trail Ridge Road within the park. The west side of the peak is in the Never Summer Wilderness, on land managed by Arapaho National Forest. Precipitation Surface runoff, runoff from the mountain's lower northwest slope drains into headwaters of the South Fork Michigan River and all other slopes drain into tributaries of the Colorado River except a portion which is diverted by the Grand Ditch. Topographic relief is significant as the summit rises above the Kawuneeche Valley in and above Baker Gulch in one-half mile. Etymology The mountain's toponym was applied in 1914 by James ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Grand Ditch
The Grand Ditch, also known as the Grand River Ditch and originally known as the North Grand River Ditch, is a water diversion project in the Never Summer Mountains, in northern Colorado in the United States. It is long, wide, and deep on average. Streams and creeks that flow from the highest peaks of the Never Summer Mountains are diverted into the ditch, which flows over the Continental Divide at La Poudre Pass at , delivering the water into Long Draw Reservoir and the Cache La Poudre River for eastern plains farmers. The water would otherwise have gone into the Colorado River (formerly known as the "Grand River", from which the name of the ditch is derived) that flows west towards the Pacific; instead, the Cache La Poudre River goes East and through the Mississippi River discharges into the Gulf of Mexico. The ditch was started in 1890 and wasn't completed until 1936. The ditch diverts between 20 and 40% of the runoff from the Never Summer Mountains, and delivers an average ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 terrain ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 terrain ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Parika Peak
Parika Peak is a mountain summit in Colorado, United States. Description Parika Peak is situated on the Continental Divide along the boundary shared by Grand County and Jackson County. It is the 13th-highest peak of the Never Summer Mountains which are a subrange of the Rocky Mountains. The west side of the peak is in the Medicine Bow–Routt National Forest and the east side is in the Never Summer Wilderness. Precipitation runoff from the mountain's slopes drains to Jack Creek and the Illinois River, with the exception of the southeast slope which drains to the Colorado River via Baker Gulch. The counterintuitive direction of water flow is because the Continental Divide forms a loop in this area, whereby the peak's west slope runoff flows to the Atlantic Ocean and the east slope to the Pacific. Topographic relief is significant as the summit rises above Jack Creek in and above Parika Lake in one-half mile (0.8 km). The summit can be reached from Parika Lake by hiking ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Baker Mountain (Colorado)
Baker Mountain is a mountain summit in Grand County, Colorado, United States. Description Baker Mountain is the 15th-highest peak of the Never Summer Mountains which are a subrange of the Rocky Mountains. The mountain is situated on the western boundary of Rocky Mountain National Park and the west side of the peak is in the Never Summer Wilderness, on land managed by Arapaho National Forest. Precipitation runoff from the mountain's slopes drains into headwaters of the Colorado River except for a portion of which is diverted by the Grand Ditch. Topographic relief is significant as the summit rises above the Kawuneeche Valley in and above Baker Gulch in 0.6 mile (1 km). History The mountain is named for John R. Baker who made the first ascent of the summit in 1875.William Bright, ''Colorado Place Names'', 2004, Johnson Books, , page 13. The mountain's toponym was officially adopted in 1932 by the United States Board on Geographic Names, and named in association with Baker ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


Mount Cumulus
Mount Cumulus is a mountain summit in Colorado, United States. Description Mount Cumulus is situated on the Continental Divide along the boundary shared by Grand County and Jackson County. It is the fourth-highest peak of the Never Summer Mountains which are a subrange of the Rocky Mountains. The mountain is situated on the western boundary of Rocky Mountain National Park and is visible from Trail Ridge Road within the park. The west side of the peak is in the Never Summer Wilderness, on land managed by Medicine Bow–Routt National Forest. Precipitation runoff from the mountain's west slope drains into headwaters of the South Fork Michigan River and the east slope drains into the Colorado River except a portion which is diverted by the Grand Ditch. The counterintuitive direction of water flow is because the Continental Divide forms a loop in this area, whereby the peak's west slope runoff flows to the Atlantic Ocean and the east slope to the Pacific. Topographic relief is s ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




Mount Cirrus
Mount Cirrus is a mountain summit in Colorado, United States. Description Mount Cirrus is situated on the Continental Divide along the boundary shared by Grand County and Jackson County. It is the third-highest peak of the Never Summer Mountains which are a subrange of the Rocky Mountains. The mountain is situated on the western boundary of Rocky Mountain National Park and is visible from Trail Ridge Road within the park. The west side of the peak is in the Never Summer Wilderness, on land managed by Medicine Bow–Routt National Forest. Precipitation runoff from the mountain's west slope drains into tributaries of the Michigan River and the east slope drains into headwaters of the Colorado River except a portion which is diverted by the Grand Ditch. The counterintuitive direction of water flow is because the Continental Divide forms a loop in this area, whereby the peak's west slope runoff flows to the Atlantic Ocean and the east slope to the Pacific. Topographic relief is ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


James Grafton Rogers
James Grafton Rogers (January 13, 1883 - April 23, 1971) was the Assistant Secretary of State for the United States. Biography Rogers was born on January 13, 1883 in Denver, Colorado to Edmund James Armstrong Rogers (1852-1922) and Maria Georgina Dare. Rogers was a professor of law and dean of the University of Colorado School of Law from 1928-1931, and 1933-35. He was the western vice president of the American Alpine Club from 1932 to 1934, and president of the American Alpine Club from 1938 to 1940. Rogers died of a stroke on April 23, 1971 in Denver, Colorado Denver () is a consolidated city and county, the capital, and most populous city of the U.S. state of Colorado. Its population was 715,522 at the 2020 census, a 19.22% increase since 2010. It is the 19th-most populous city in the Unit .... References {{DEFAULTSORT:Rogers, James Grafton 1883 births 1971 deaths United States Assistant Secretaries of State University of Colorado Boulder facu ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]