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Mount Majestic (Utah)
Mount Majestic, also known as Majestic Mountain, is a elevation Navajo Sandstone double-summit mountain located in Zion National Park, in Washington County, Utah, Washington County of southwest Utah, United States. Description Mount Majestic is situated near the north end of Zion Canyon, towering above the canyon floor and the North Fork Virgin River, which drains precipitation Surface runoff, runoff from this mountain. Majestic is the parent to Cathedral Mountain (Zion), Cathedral Mountain, with only 0.24 mile of separation between them. Other neighbors include The Great White Throne, Observation Point (Zion), Observation Point, Red Arch Mountain, Lady Mountain, Castle Dome (Zion), Castle Dome, Cable Mountain, and Angels Landing. 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 Mount Majestic. According to the Köppen climate classification system, it is located in a Cold ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zion National Park
Zion National Park is an American national park located in southwestern Utah near the town of Springdale. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the park has a unique geography and a variety of life zones that allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals (including 19 species of bat), and 32 reptiles inhabit the park's four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches. The lowest point in the park is at Coalpits Wash and the highest peak is at Horse Ranch Mountain. A prominent feature of the park is Zion Canyon, which is long and up to deep. The canyon walls are reddish and tan-colored Navajo Sandstone eroded by the North Fork of the Virgin River. Human habitation of the area started about 8,000 years ago with small ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Observation Point (Zion)
Observation Point is a elevation Navajo Sandstone feature located in Zion National Park, in Washington County of southwest Utah, United States. Observation Point is situated at the north end of Zion Canyon, towering above the canyon floor and the North Fork of the Virgin River which drains precipitation runoff from this viewpoint. A popular 8-mile round-trip trail climbs from the Weeping Rock trailhead along Zion Canyon Road to reach the top.Erik Molvar and Tamara Martin, ''Hiking Zion and Bryce Canyon National Parks'', Second Edition, Globe Pequot Press, 2005, page 56. Neighbors visible from the point include The Great White Throne, Cathedral Mountain, Angels Landing, and Cable Mountain. This geographical 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 Observation Point. According to the Köppen climate classification system, it is located in a Cold semi-arid climate zone, whi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone Formations Of The United States
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topography, topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porosity, porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism ... [...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] |
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] |
Angels Landing
Angels Landing, known previously as the Temple of Aeolus, is a tall Formation of rocks, rock formation in Zion National Park in southwestern Utah, United States. A renowned trail cut into solid rock in 1926 leads to the top of Angels Landing and provides panoramic views of Geology of the Zion and Kolob canyons area, Zion Canyon. Trail The trail to Angels Landing is long with an approximate elevation gain. The hike is rated as a class 3 difficulty based on the Yosemite Decimal System. It begins at the Grotto drop off point on the park's shuttle system, which operates from early spring through late fall. It roughly follows the path of the Virgin River for some time along the West Rim Trail, slowly gaining elevation in sandy terrain. Most of the trail is uphill on the way up to Angels Landing. As the trail gets steeper and leaves behind the river, it becomes paved. After a series of steep Hairpin turn, switchbacks, the trail goes through the area between Angels Landing and the Zi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cable Mountain
Cable Mountain is a elevation Navajo Sandstone summit located in Zion National Park, in Washington County of southwest Utah, United States. Towering above the floor of Zion Canyon at the Big Bend area, Cable Mountain is situated immediately northeast of The Great White Throne, separated by the chasm of Hidden Canyon. It is set on the east side of the North Fork Virgin River which drains precipitation runoff from this mountain. Its neighbors include Angels Landing, Cathedral Mountain, The Organ, and Observation Point. This mountain's name was officially adopted in 1934 by the U.S. Board on Geographic Names. It is so named in association with the draw-works which used cables to lower timber from the top of the plateau down to the valley bottom from 1901 through 1927. Wood to construct the Zion Lodge came down the cable works. A 7.4-mile trail, much of it an old wagon road, leads to the views from the top.Greg Witt, ''50 Best Short Hikes Utah's National Parks'', 2nd Edition, W ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Castle Dome (Zion)
Castle Dome is a elevation Navajo Sandstone summit located in Zion National Park, in Washington County of southwest Utah, United States. Castle Dome is situated northwest of Zion Lodge, towering above the lodge and the floor of Zion Canyon. It is set on the west side of the North Fork Virgin River which drains precipitation runoff from this mountain. It is wedged between Behunin Canyon and Heaps Canyon, with the popular Emerald Pools set at the southeast foot of this mountain. Its neighbors include Mount Majestic, Cathedral Mountain, The Great White Throne, Red Arch Mountain, Mountain of the Sun, and Lady Mountain. 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 Castle Dome. 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), ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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