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Red Arch Mountain
Red Arch Mountain is a elevation Navajo Sandstone summit located in Zion National Park, in Washington County of southwest Utah, United States. Description Red Arch Mountain is situated immediately northeast of Zion Lodge, towering above the lodge and the floor of Zion Canyon. It is set on the east 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, Mountain of the Sun, Mount Moroni, and Lady Mountain. This mountain's descriptive name was officially adopted in 1934 by the U.S. Board on Geographic Names. It is so named for a blind arch that formed in 1880 on the northwest face when a rock avalanche fell into the valley. This event buried the Gifford farm in rubble. It happened on a Sunday when the family was away at church in Springdale. Climate Spring and fall are the most favorable seasons to visit Red Arch Mountain. According to the Köppen climate ... [...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] |
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] |
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] |
Rock Avalanche
A rockslide is a type of landslide caused by rock failure in which part of the bedding plane of failure passes through compacted rock and material collapses ''en masse'' and not in individual blocks. Note that a rockslide is similar to an avalanche because they are both slides of debris that can bury a piece of land. While a landslide occurs when loose dirt or sediment falls down a slope, a rockslide occurs only when solid rocks are transported down slope. The rocks tumble downhill, loosening other rocks on their way and smashing everything in their path. Fast-flowing rock slides or debris slides behave similarly to snow avalanches, and are often referred to as rock avalanches or debris avalanches. Definition The term landslide refers to a variety of mass wasting events (geologic slope failures) that include slumps, slides, falls, and flows. The two major types of slides are rotational slides and translational slides. Rockslides are a type of translational event since the rock ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Natural Arch
A natural arch, natural bridge, or (less commonly) rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs, coastal cliffs, fins or stacks are subject to erosion from the sea, rivers or weathering ( subaerial processes). Most natural arches are formed from narrow fins and sea stacks composed of sandstone or limestone with steep, often vertical, cliff faces. The formations become narrower due to erosion over geologic time scales. The softer rock stratum erodes away creating rock shelters, or alcoves, on opposite sides of the formation beneath the relatively harder stratum, or caprock, above it. The alcoves erode further into the formation eventually meeting underneath the harder caprock layer, thus creating an arch. The erosional processes exploit weaknesses in the softer rock layers making cracks larger and removing material more quickly than the caprock; however, the caprock itself continues to er ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blind Arch
A blind arch is an arch found in the wall of a building that has been infilled with solid construction and so cannot serve as a passageway, door or window.''A Dictionary of Architecture''; Fleming, John; Honour, Hugh & Pevsner, Nikolaus (1966) The term is most often associated with masonry wall construction, but blind arches are also found (or simulated) in other types of construction such as light frame construction. Some blind arches were originally built as open arches and infilled later. Others were originally built with solid infill as intentional stylistic elements. See also * Blind arcade * Lombard band * Lesene A lesene, also called a pilaster strip, is an architectural term for a narrow, low-relief vertical pillar on a wall. It resembles a pilaster, but does not have a base or capital. It is typical in Lombardic and Rijnlandish architectural building ... References External links Description and photo [...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] |
