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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] |
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] |
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] |
Headframe
A headframe (also known as a gallows frame, winding tower, hoist frame,Ernst, Dr.-Ing. Richard (1989). ''Wörterbuch der Industriellen Technik'' (5th ed.). Wiesbaden: Oscar Brandstetter, 1989. pit frame, shafthead frame, headgear, headstock or poppethead) is the structural frame above an underground mine shaft so as to enable the hoisting of machinery, personnel, or materials. Design Modern headframes are built out of steel, concrete or a combination of both. Timber headframes are no longer used in industrialized countries, but are still used in developing nations. Conventionally steel headframes are used when a drum hoist is employed, and concrete headframes are built for friction hoists; however a steel headframe can be used with a friction hoist for shafts with a smaller capacity and depth. Steel headframes A steel headframe is less expensive than a concrete headframe; the tallest steel headframe measures 87 m. Steel headframes are more adaptable to modifications (mak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brigham Young
Brigham Young (; June 1, 1801August 29, 1877) was an American religious leader and politician. He was the second President of the Church (LDS Church), president of the Church of Jesus Christ of Latter-day Saints (LDS Church), from 1847 until his death in 1877. During his time as church president, Young led his followers, the Mormon pioneers, west from Nauvoo, Illinois, to the Salt Lake Valley. He founded Salt Lake City and served as the first governor of the Utah Territory. Young also worked to establish the learning institutions which would later become the University of Utah and Brigham Young University. A Polygamy and the Latter Day Saint movement, polygamist, Young had at least 56 wives and 57 children. He Black people and Mormon priesthood, instituted a ban prohibiting conferring the Black people and early Mormonism, priesthood on men of black African descent, and led the church in the Utah War against the United States Armed Forces, United States. Early life Young was born ... [...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] |
Zion Lodge
Zion Lodge is located in Zion National Park, Utah, United States. The lodge was designed in 1924 as a compromise solution between its developer, the Utah Parks Company, which wanted a large hotel, and National Park Service director Stephen Mather, who desired smaller-scale development. The Utah Parks Company had been formed in 1923 as a subsidiary of the Union Pacific Railroad, and was, like many similar programs, intended to stimulate passenger rail traffic to the national parks of southwest Utah. Gilbert Stanley Underwood designed the Zion Lodge as part of a series of similar structures for the Utah Parks Company at the north rim of the Grand Canyon and at Bryce Canyon National Park. Underwood's design was more modest in scale and detailing than those at the Grand Canyon and Bryce, substituting milled lumber for whole logs in a "studs-out" style. Underwood used less stonework, in smaller pieces. The structures were designed to be more in keeping with the character of the valle ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Draw-works
A drawworks is the primary hoisting machinery component of a rotary drilling rig. Its main function is to provide a means of raising and lowering the traveling block. The wire-rope drill line winds on the drawworks drum and over the crown block to the traveling block, allowing the drill string to be moved up and down as the drum turns. The segment of drill line from the drawworks to the crown block is called the "fast line". The drill line then enters the first sheave of the crown block and makes typically 6 to 12 passes between the crown block and traveling block pulleys for mechanical advantage. The line then exits the last sheave on the crown block and is fastened to a derrick leg on the other side of the rig floor. This section of drill line is called the "dead line." A modern drawworks consists of five main parts: the drum, the power source, the reduction gear, the brake, and the auxiliary brake. The apparatus can be powered by AC or DC, or the drawworks may be conne ... [...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] |
