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The Sundial (Zion)
The Sundial is a elevation white Navajo Sandstone summit located in Zion National Park, in Washington County of southwest Utah, United States. Description The Sundial is situated in the "Towers of the Virgin", west of Zion's park headquarters, towering above the floor of Zion Canyon and the Virgin River which drains precipitation runoff from this mountain. Its nearest higher neighbor is The West Temple, one half mile to the southeast, and Altar of Sacrifice is set approximately one mile to the north-northeast. Other neighbors include The Witch Head, Bee Hive, The Sentinel, Mount Spry, Bridge Mountain, and Mount Kinesava. This geographical feature was named by the park's third superintendent, Preston P. Patraw, because it had long been used as a sundial to regulate clocks in the nearby town of Grafton. The Sundial'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 The Sundial. Accor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The West Temple
The West Temple is a prominent 7,810-foot (2,380 m) mountain summit composed of Navajo Sandstone in Zion National Park in Washington County of Utah, United States. This, the highest feature in Zion Canyon, was originally called "''Temp-o-i-tin-car-ur''" meaning "Mountain without a trail" by the Paiute people. It was called ''Steamboat Mountain'' by local Mormon settlers before 1934, when the USGS officially changed it to its present name, which was applied by John Wesley Powell during his explorations in 1872. West Temple is situated two miles northwest of Springdale, Utah, one mile northeast of Mount Kinesava, and two miles west of the park headquarters. It is one of the notable landmarks in the park. The nearest higher peak is Windy Peak, to the north. Precipitation runoff from the mountain drains into tributaries of the Virgin River. Climbing Routes Climbing Routes on The West Temple * Southwest Ridge - - 10 pitches * ''Back Where It All Begins'' - - 16 pitches * ''Big Lebo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bee Hive (peak)
Bee Hive is a Navajo Sandstone mountain in Zion National Park in Washington County, Utah, United States, that is part of the Towers of the Virgin. Description Bee Hive is located north of the park headquarters at the south entrance to Zion Canyon. The east face of Bee Hive, named The Streaked Wall, rises above the floor of Zion Canyon, and is a venue for big wall climbing. Neighbors include Altar of Sacrifice and Meridian Tower to the west, and The Sentinel to the northeast. The peak's descriptive name is for the beehive shape of the summit. This name was officially adopted in 1934 by the U.S. Board on Geographic Names. Precipitation runoff from the mountain drains into the North Fork Virgin River. Climate Spring and fall are the most favorable seasons to see Bee Hive Peak. 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), and ... [...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] |
Grafton, Utah
Grafton is a ghost town, just south of Zion National Park in Washington County, Utah, United States. Said to be the most photographed ghost town in the West, it has been featured as a location in several films, including 1929's ''In Old Arizona''—the first talkie filmed outdoors—and the classic ''Butch Cassidy and the Sundance Kid''. The nearest inhabited town is Rockville. History The site was first settled in December 1859 as part of a southern Utah cotton-growing project ordered by Brigham Young (see Utah's Dixie). A group from Virgin led by Nathan Tenney established a new settlement they called Wheeler. Wheeler didn't last long; it was largely destroyed on the night of January 8, 1862 by a weeks-long flood of the Virgin River, part of the Great Flood of 1862. The rebuilt town, about a mile upriver, was named New Grafton, after Grafton, Massachusetts. The town grew quickly in its first few years. There were some 28 families by 1864, each farming about an acre (0 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sundial
A sundial is a horological device that tells the time of day (referred to as civil time in modern usage) when direct sunlight shines by the apparent position of the Sun in the sky. In the narrowest sense of the word, it consists of a flat plate (the ''dial'') and a gnomon, which casts a shadow onto the dial. As the Sun appears to move through the sky, the shadow aligns with different hour-lines, which are marked on the dial to indicate the time of day. The ''style'' is the time-telling edge of the gnomon, though a single point or ''nodus'' may be used. The gnomon casts a broad shadow; the shadow of the style shows the time. The gnomon may be a rod, wire, or elaborately decorated metal casting. The style must be parallel to the axis of the Earth's rotation for the sundial to be accurate throughout the year. The style's angle from horizontal is equal to the sundial's geographical latitude. The term ''sundial'' can refer to any device that uses the Sun's altitude or azimut ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Kinesava
Mount Kinesava is a sandstone mountain summit located in Zion National Park, in Washington County of southwest Utah, United States. Description Mount Kinesava is located immediately west of Springdale, towering above the town and the floor of Zion Canyon. Precipitation runoff from this mountain drains into tributaries of the Virgin River. Its nearest higher neighbor is The West Temple, to the northeast. Other notable mountains wthin view from the summit include The Watchman to the east-southeast, Bridge Mountain to the east-northeast, and Mount Spry is positioned to the northeast. This feature's name was officially adopted in 1934 by the U.S. Board on Geographic Names. It is so named for ''Kinesava'', the Paiute deity of trickery. Climate Spring and fall are the most favorable seasons to visit Mount Kinesava. 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 m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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