|
The Organ (Zion)
The Organ is a elevation Navajo Sandstone summit located in Zion National Park, in Washington County of southwest Utah, United States. The Organ is situated in the Big Bend at the north end of Zion Canyon, rising 700-feet (213 meters) above the canyon floor and the North Fork of the Virgin River which drains precipitation runoff from this rock. Neighbors include The Great White Throne, Cathedral Mountain, Angels Landing, Observation Point, and Cable Mountain. The Organ is believed to have been named by Claud Hirschi and Ethelbert Bingham, residents of Rockville, on their 1916 trip with Methodist Minister Frederick Vining Fisher, who also named geographical formations in Zion. This geographical feature's descriptive 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 The Organ. 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] |
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 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] |
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] |
Rockville, Utah
Rockville is a town in Washington County, Utah, United States. It is located along the Virgin River near the mouth of Zion Canyon. The city lies just outside the park boundary for Zion National Park; the park entrance is located approximately 5 miles (8 km) northeast of the town. Geography According to the United States Census Bureau, the town has a total area of 8.4 square miles (21.8 km2), all land. Climate Rockville experiences warm and dry summers, with summer monthly averages around 75 F°, and average highs around 90 F°. The town has winter averages around 35 F°, and average lows around 23 F°. The town experiences relatively low annual precipitation, with a yearly average of 13.2" precipitation. According to the Köppen Climate Classification system, Rockville has a warm-summer Mediterranean climate, abbreviated "Csb" on climate maps. Demographics As of the census of 2010, there were 245 people, 119 households, and 63 families residing in the town. The ... [...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] |
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] |
Cathedral Mountain (Zion)
Cathedral Mountain is a elevation Navajo Sandstone summit located in Zion National Park, in Washington County of southwest Utah, United States. Description Cathedral Mountain 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 mountain. Cathedral is the nearest higher neighbor to Angels Landing, with of separation, and the Angels Landing Trail traverses Refrigerator Canyon between them. Other neighbors include The Great White Throne, Observation Point, The Organ, Lady Mountain, Cable Mountain, and parent Mount Majestic. This feature's descriptive name was applied by Stephen S. Johnson in 1922, and officially adopted in 1934 by the U.S. Board on Geographic Names. ''The Spearhead'', elevation 5,804-ft, is the southernmost tip of this mountain, and is prominently featured from Zion Lodge. The first ascent of Cathedral was made by Walter Becker, Fritz Becker, and Rudolph ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Great White Throne
The Great White Throne is a monolith, predominantly composed of white Navajo Sandstone in Zion National Park in Washington County in southwestern Utah, United States. The north-west "main" face rises in from the floor of Zion Canyon near Angels Landing. It is often used as a symbol of Zion National Park. The Great White Throne can be seen from most locations along the scenic drive running through Zion Canyon. Naming The Great White Throne was named by the Methodist minister of Ogden, Utah, Frederick Vining Fisher, in 1916.''A History of Southern Utah and Its National Parks'', Angus M. Woodbury (Utah State Historical Society, Vol XII Nos. 3–4, July–October 1944; revised and reprinted, 1950: pages 198-199 ) On a trip up the canyon with Claud Hirschi, Fisher and Hirschi named many features in Zion Canyon. Later afternoon light gloriously lit up The Great White Throne, prompting Fischer to state: Climbing regulations A bivouac permit is required from the park visitor cent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Virgin River
The Virgin River is a tributary of the Colorado River in the U.S. states of Utah, Nevada, and Arizona. The river is about long.Calculated with Google Maps and Google Earth It was designated Utah's first wild and scenic river in 2009, during the centennial celebration of Zion National Park. History The first known Euro-American party to encounter the Virgin was led by Jedediah Smith in 1826. Smith named it "Adams River", after then-president John Quincy Adams.Smith, Jedediah S., arrison G. Rogers and George R. Brooks (ed.). ''The Southwest Expedition of Jedediah S. Smith: His Personal Account of the Journey to California, 1826–1827'', p. 55. Lincoln and London, University of Nebraska Press, 9771989. Later explorer and mapmaker John C. Fremont reported that it was called "Rio Virgen" but did not state the origin of the name. Hiram Chittenden speculated that Smith had later renamed the river after Thomas Virgin, who was badly wounded in an 1827 attack by Mohave people during ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
