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Cathedral Mountain (Zion National Park)
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 Rudo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
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] |
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] |
First Ascent
In mountaineering, a first ascent (abbreviated to FA in guide books) is the first successful, documented attainment of the top of a mountain or the first to follow a particular climbing route. First mountain ascents are notable because they entail genuine exploration, with greater risks, challenges and recognition than climbing a route pioneered by others. The person who performs the first ascent is called the first ascensionist. In free climbing, a first ascent (or first free ascent, abbreviated FFA) of a climbing route is the first successful, documented climb of a route without using equipment such as anchors or ropes for aiding progression or resting. History The details of the first ascents of even many prominent mountains are scanty or unknown; sometimes the only evidence of prior summiting is a cairn, artifacts, or inscriptions at the top. Today, first ascents are generally carefully recorded and usually mentioned in guidebooks. The term is also used when referrin ... [...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] |
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 Editio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lady Mountain
Lady Mountain (previously known as Cliff Dwelling Mountain) is a elevation Navajo Sandstone summit located in Zion National Park, in Washington County of southwest Utah, United States. Description Lady Mountain is situated immediately west of Zion Lodge, towering over 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. Its neighbors include Mount Majestic, Cathedral Mountain, The Great White Throne, Red Arch Mountain, Mountain of the Sun, Mount Moroni, Castle Dome, and The Sentinel. This feature was called "Cliff Dwelling Mountain" and "Mount Zion" before the Lady Mountain name was officially adopted in 1934 by the U.S. Board on Geographic Names. It is so named for markings of which early visitors saw a resemblance to a lady's face. In 1925 the park service constructed a climbing "trail" with cables and ladders to the summit, one of the first in the park, but it was ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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