Hayden Spire
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Hayden Spire
Hayden Spire is a 12,480+ foot elevation (3,800 meter) pillar located in Rocky Mountain National Park, in Larimer County, Colorado, Larimer County, Colorado, United States. It is situated 12 miles west of the community of Estes Park, Colorado, Estes Park in Hayden Gorge, along a short spur on the Continental Divide of the Americas, Continental Divide. Hayden Spire is part of the Front Range which is a subset of the Rocky Mountains. It is the highest tower in a cluster of spires which can be viewed from Forest Canyon Overlook along the Trail Ridge Road. Topographic relief is significant as the north aspect rises above Hayden Gulch in one-half mile. Neighbors include Terra Tomah Mountain two miles to the north, and Mount Julian (Colorado), Mount Julian 1.8 mile to the northwest. Climate According to the Köppen climate classification system, Hayden Spire is located in an alpine subarctic climate zone with cold, snowy winters, and cool to warm summers. Due to ...
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Sprague Mountain
Sprague Mountain is a mountain summit on the boundary shared by Grand County, Colorado, Grand County and Larimer County, Colorado, Larimer County, in Colorado, United States. It is set on the Continental Divide in the Front Range of the Rocky Mountains, and west of the community of Estes Park, Colorado, Estes Park. Precipitation Surface runoff, runoff from the mountain's east side drains into tributaries of the Big Thompson River and the west slope drains into headwaters of Tonahutu Creek which flows to Grand Lake (Colorado), Grand Lake. Topographic relief is significant as the summit rises over above Tonahutu Creek in one mile. The peak is visible from Trail Ridge Road. Etymology Abner E. Sprague, Abner Erwin Sprague (1850–1943) was one of the early settlers of Estes Park who homesteaded in the nearby Moraine Park area in 1874. Other landforms in the national park bearing his name include Sprague Lake (Colorado), Sprague Lake, Sprague Glacier, and Sprague Pass. The mounta ...
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Topographic Relief
Terrain (), alternatively relief or topographical relief, is the dimension and shape of a given surface of land. 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. Bathymetry is the study of underwater relief, while hypsometry studies terrain relative to sea level. 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, drainage characteristics, drainage systems, groundwater systems, water ...
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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 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 climate, mountains te ...
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United States Board On Geographic Names
The United States Board on Geographic Names (BGN) is a Federal government of the United States, federal body operating under the United States Secretary of the Interior. The purpose of the board is to establish and maintain uniform usage of geography, geographic names throughout the federal government of the United States. History Following the American Civil War, more and more American pioneer, American settlers began moving westward, prompting the Federal government of the United States, U.S. federal government to pursue some sort of consistency for referencing landmarks on maps and in official documents. As such, on January 8, 1890, Thomas Corwin Mendenhall, superintendent of the United States 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 si ...
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Abner E
In the Hebrew Bible, Abner ( ) was the cousin of King Saul and the commander-in-chief of his army. His name also appears as "Abiner son of Ner", where the longer form Abiner means "my father is Ner". Biblical narrative Abner is initially mentioned incidentally in Saul's history, first appearing as the son of Ner, Saul's uncle, and the commander of Saul's army. He then comes to the story again as the commander who introduced David to Saul following David's killing of Goliath. He is not mentioned in the account of the disastrous battle of Gilboa when Saul's power was crushed. Seizing the youngest but only surviving of Saul's sons, Ish-bosheth, also called Eshbaal, Abner set him up as king over Israel at Mahanaim, east of the Jordan. David, who was accepted as king by Judah alone, was meanwhile reigning at Hebron, and for some time war was carried on between the two parties. The only engagement between the rival factions told at length was preceded by an encounter at Gibeon be ...
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Hayden Spire, Rocky Mountain NP
Hayden may refer to: Places Inhabited places in the United States *Hayden, Alabama *Hayden, Arizona *Hayden's Ferry, former name of Tempe, Arizona *Hayden, California, former name of Hayden Hill, California *Hayden, Colorado *Hayden, Idaho *Hayden Lake, Idaho * Hayden, Indiana * Hayden Island, Portland, Oregon, an island and neighborhood Geographic features in the United States *Hayden Butte or Tempe Butte, an andesite butte of volcanic origin in Tempe, Arizona * Hayden Creek (other) * Hayden Mountain (other) * Hayden Peak (Utah), a mountain in Utah * Hayden Valley, a large sub-alpine valley in Yellowstone National Park Other places * Hayden, Gloucestershire, a village in the UK People and fictional characters * Hayden (given name), including a list of people and fictional characters *Hayden (surname), including a list of people and fictional characters *Hayden (musician) (born 1971), a Canadian folk musician Other uses *Hayden (electronics company), a Britis ...
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Big Thompson River
The Big Thompson River is a tributary of the South Platte River, approximately 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 Canyon. From Lake Es ...
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Surface Runoff
Surface runoff (also known as overland flow or terrestrial runoff) is the unconfined flow of water over the ground surface, in contrast to ''channel runoff'' (or ''stream flow''). It occurs when excess rainwater, stormwater, meltwater, or other sources, can no longer sufficiently rapidly infiltrate in the soil. This can occur when the soil is #Saturation excess overland flow, saturated by water to its full capacity, and the rain arrives #Infiltration excess overland flow, more quickly than the soil can absorb it. Surface runoff often occurs because wikt:impervious#Adjective, impervious areas (such as roofs and Road surface, pavement) do not allow water to soak into the ground. Furthermore, runoff can occur either through natural or human-made processes. Surface runoff is a major component of the water cycle. It is the primary agent of Soil erosion#Rainfall and runoff, soil erosion by water. The land area producing runoff that drains to a common point is called a drainage basin. ...
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Subarctic Climate
The subarctic climate (also called subpolar climate, or boreal climate) is a continental 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°N to 70°N, poleward of the humid continental climates. Like other Class D climates, they are rare in the Southern Hemisphere, only found at some isolated highland elevations. 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 on ...
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Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. 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'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ...
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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, 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 This is a list of the 64 counties of the U.S. State of Colorado by their points of highest elevation. Of the 50 highest county high points in the United States, 30 are located in Colorado. The highest point in Colorado and the Rocky Mountai ... References External links Mountains of Rocky Mountain National Park Mountains of Larimer County, Colorado Three-thousa ...
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