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Terra Tomah Mountain
Terra Tomah Mountain is a mountain summit located in Rocky Mountain National Park, in Larimer County, of Colorado, United States. It is situated 13 miles west of the community of Estes Park, and 1.5 mile east of the Continental Divide. Terra Tomah Mountain is part of the Front Range which is a subset of the Rocky Mountains. Topographic relief is significant as the northeast aspect rises above Forest Canyon in 1.5 mile. It is a prominent landmark viewed from Forest Canyon Overlook along the Trail Ridge Road. Etymology In 1914 George Barnard was hiking here with the Colorado Mountain Club. Inspired by a lake, he chanted a Cahuilla ghost dance song with the lyrics "terra toma", which was popular among students at Pomona College where he attended. The president of the club, James Grafton Rogers, submitted the name for the lake to the federal government for consideration. However, the government erred by applying this name to the mountain instead. In 1923 the club listed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Julian (Colorado)
Mount Julian is a mountain summit in the northern Front Range of the Rocky Mountains of North America. The peak is located in the Rocky Mountain National Park Wilderness, west ( bearing 268°) of the Town of Estes Park in Larimer County Larimer County is a county located in the U.S. state of Colorado. As of the 2020 census, the population was 359,066. The county seat and most populous city is Fort Collins. The county was named for William Larimer, Jr., the founder of Den ..., Colorado, United States. The mountain was named in honor of Julian Hayden, a civil engineer who lived in Estes Park. 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 Larimer County, Colorado Nor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ghost Dance
The Ghost Dance ( Caddo: Nanissáanah, also called the Ghost Dance of 1890) was a ceremony incorporated into numerous Native American belief systems. According to the teachings of the Northern Paiute spiritual leader Wovoka (renamed Jack Wilson), proper practice of the dance would reunite the living with spirits of the dead, bring the spirits to fight on their behalf, end American westward expansion, and bring peace, prosperity, and unity to Native American peoples throughout the region. The basis for the Ghost Dance is the circle dance, a traditional Native American dance. The Ghost Dance was first practiced by the Nevada Northern Paiute in 1889. The practice swept throughout much of the Western United States, quickly reaching areas of California and Oklahoma. As the Ghost Dance spread from its original source, different tribes synthesized selective aspects of the ritual with their own beliefs. The Ghost Dance was associated with Wovoka's prophecy of an end to colonial expan ... [...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 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Thompson Cany ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
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] |
David Prescott Barrows
David Prescott Barrows (June 27, 1873 – September 5, 1954) was an American anthropologist, explorer, and educator. Born in Chicago in 1874, his family moved to California. He showed a keen interest in the life and customs of Native Americans, and was said to have "spent almost every summer during the period 1890–1899 in research work among the tribes of southern California and in the Colorado Desert." He later became President of the University of California. He traveled extensively, publishing descriptions of his findings in countries such as Morocco and the Philippines. Early years Barrows graduated from Pomona College in 1894, where he served as the founding editor of its newspaper, ''The Student Life''. He then obtained a Master's degree in political science from the University of California, Berkeley in 1895. During the summers between 1890 and 1899 he pursued research with the tribes of southern California and the Colorado Desert, and wrote a thesis on "the Ethno-Botany ... [...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 ques ... [...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 A stroke is a medical condition in which poor blood flow to the brain causes cell death. There are two main types of stroke: ischemic, due to lack of blood flow, and hemorrhagic, due to bleeding. Both cause parts of the brain to stop functionin ... on April 23, 1971 in Denver, Colorado. References {{DEFAULTSORT:Rogers, James Grafton 1883 births 1971 deaths United States Assistant Secretaries of State University of Colorado Boulder ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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