|
Twin Brothers (film)
Twin Brothers is a Navajo Sandstone mountain in Zion National Park in Washington County , Utah, United States. Description Twin Brothers is situated immediately north of The East Temple, and immediately south of Mountain of the Sun, towering above the floor of Zion Canyon. It is set on the east side of the North Fork of the Virgin River which drains precipitation runoff from this mountain. Its neighbors across the canyon include Bee Hive, The Sentinel, and Mount Moroni. Mount Spry, set southwest and below Twin Brothers, often appears in photos taken of both from park headquarters. This feature's name was officially adopted in 1934 by the U.S. Board on Geographic Names. Climate Spring and fall are the most favorable seasons to visit Twin Brothers. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is defined by the coldest month having an average mean temperature below 32 °F (0 °C), and at least 50% of the total ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The East Temple
The East Temple is a prominent summit composed of Navajo Sandstone in Zion National Park, in Washington County of southwest Utah, United States. It is one of the notable landmarks in the park. The nearest neighbor is Twin Brothers, one-half mile to the north, and the nearest higher peak is The West Temple, to the west-southwest. The mountain is situated 1.8 miles northeast of the park headquarters, at the confluence of Pine Creek and the North Fork Virgin River. This feature's name was applied by John Wesley Powell during his explorations in 1872, and was officially adopted in 1934 by the U.S. Board on Geographic Names. The first ascent was made in 1937 by Glen Dawson, Dick Jones, Homer Fuller, Wayland Gilbert, and Jo Momyer. Climbing Routes Climbing Routes on The East Temple Mountain Project * Casual Route - - 4 pit ... [...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] |
Mountains Of Washington County, Utah
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] |
Mountains Of Utah
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] |
Geology Of The Zion And Kolob Canyons Area
The geology of the Zion and Kolob canyons area includes nine known exposed formations, all visible in Zion National Park in the U.S. state of Utah. Together, these formations represent about 150 million years of mostly Mesozoic-aged sedimentation in that part of North America. Part of a super-sequence of rock units called the Grand Staircase, the formations exposed in the Zion and Kolob area were deposited in several different environments that range from the warm shallow seas of the Kaibab and Moenkopi formations, streams and lakes of the Chinle, Moenave, and Kayenta formations to the large deserts of the Navajo and Temple Cap formations and dry near shore environments of the Carmel Formation. Subsequent uplift of the Colorado Plateau slowly raised these formations much higher than where they were deposited. This steepened the stream gradient of the ancestral rivers and other streams on the plateau. The faster-moving streams took advantage of uplift-created joints in the rock ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains In Utah
Mountains in Utah are numerous and have varying elevations and prominences. Kings Peak, in the Uinta Mountains in Duchesne County, Utah, is the highest point in the state and has the greatest prominence. It has elevation and prominence . It also has topographic isolation of , highest amongst summits of Utah having at least 500 meters of prominence. For lists of the top 50 peaks in Utah by elevation, prominence, and topographic isolation, see List of mountain peaks of Utah. This "List of mountains in Utah" should include all of those (but does not yet) and more. To see locations of all mountains having coordinates in this article (primarily from just three counties in the state, so far) together in one map, click on "Map all coordinates using OSM" at the right side of this page. Partial lists of mountains in just a few of Utah's 29 counties are below. Salt Lake County Mountains in Salt Lake County, Utah include: Utah County Mountains in Utah County, Utah i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deertrap Mountain
Deertrap Mountain is a mountain in Zion National Park in Washington County, Utah, United States. Description Deertrap Mountain is composed of white Navajo Sandstone and set on the east rim of Zion Canyon. It is situated one mile southeast of Zion Lodge, and three miles northeast of park headquarters. The nearest neighbor is Mountain of the Sun, one-half mile to the west, and the nearest higher peak is Twin Brothers, to the southwest. The East Temple is situated 1.1 mile to the south-southwest, and Ant Hill is set to the southeast. Pine Creek originates at Deertrap, and the North Fork of the Virgin River drains precipitation runoff from this mountain. This feature's name was officially adopted April 4, 1934, by the U.S. Board on Geographic Names. It is believed that the Paiute drove mule deer onto the mesa here, trapping them for food. Climate Spring and fall are the most favorable seasons to visit Deertrap Mountain. According to the Köppen climate classification system, it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cold Semi-arid Climate
A semi-arid climate, semi-desert climate, or steppe climate is a dry climate sub-type. It is located on regions that receive precipitation below potential evapotranspiration, but not as low as a desert climate. There are different kinds of semi-arid climates, depending on variables such as temperature, and they give rise to different biomes. Defining attributes of semi-arid climates A more precise definition is given by the Köppen climate classification, which treats steppe climates (''BSk'' and ''BSh'') as intermediates between desert climates (BW) and humid climates (A, C, D) in ecological characteristics and agricultural potential. Semi-arid climates tend to support short, thorny or scrubby vegetation and are usually dominated by either grasses or shrubs as it usually can't support forests. To determine if a location has a semi-arid climate, the precipitation threshold must first be determined. The method used to find the precipitation threshold (in millimeters): *multiply ... [...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] |
Mount Spry
} Mount Spry is a small 5,720-ft elevation mountain summit made of Navajo Sandstone located in Zion National Park, in Washington County of southwest Utah, United States. Officially named in 1934, it honors William Spry (1864-1929), the third governor of Utah. The nearest higher peak is The East Temple, to the east. Precipitation runoff from the mountain drains into tributaries of the North Fork Virgin River. Climbing Routes Climbing Routes on Mount Spry Mountain Project * ''Holy Roller'' - - 5 pitches * ''Swamp Donkey'' - - 5 pitches * ''Shark Tooth Freighter'' - - 3 pitches Climate Spring and fall are the most favorable seasons to visit Mount Spry. According to the |
Mount Moroni
Mount Moroni is a elevation Navajo Sandstone summit located at the Court of the Patriarchs in Zion National Park, in Washington County of southwest Utah, United States. Description Mount Moroni is located immediately southwest of Zion Lodge, towering above the lodge and the floor of Zion Canyon. It is set alongside the North Fork of the Virgin River which drains precipitation runoff from this mountain. Its neighbors include The Sentinel, Mountain of the Sun, Twin Brothers, Mount Spry, The East Temple, and the Three Patriarchs: peaks Abraham, Isaac, and Jacob. This feature's name was officially adopted in 1934 by the U.S. Board on Geographic Names. It is named for Angel Moroni, who presented Joseph Smith with the golden plates from which he translated and published the Book of Mormon. Climate Spring and fall are the most favorable seasons to visit Mount Moroni. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, which is de ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Sentinel (Zion National Park)
The Sentinel is a elevation Navajo Sandstone summit located near the Court of the Patriarchs in Zion National Park, in Washington County of southwest Utah, United States, that is part of the Towers of the Virgin. The national park map lists the elevation as 7,157-feet. Description The Sentinel is located north of Zion's park headquarters, towering above the park road and the floor of Zion Canyon. It is set alongside the North Fork of the Virgin River which drains precipitation runoff from this mountain. Its neighbors include Bee Hive, Mount Spry, The East Temple, Mount Moroni, Mountain of the Sun, Twin Brothers, and the Three Patriarchs. This feature's name was officially adopted in 1934 by the U.S. Board on Geographic Names. In 1995, a landslide at the base of The Sentinel dammed the Virgin River and washed out a section of the park road. The Sentinel was once much bigger before a huge rock avalanche fell from it, when 4,800 years ago the Sentinel Slide with a volume of 286 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
