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Burbank Hills
The Burbank Hills are a small northwest-southeast mountain range in western Utah, United States that lie entirely within the Hamlin-Snake Watershed, between the Snake Range and the Ferguson Desert. It is bounded by Snake Valley to the north, west, and south; and trends into the Tunnel Springs Mountains, to the southeast, opposite the Antelope Valley on its southeast border. It was named after the settlement of Burbank, Utah, and Margie Burbank Clay, the wife of local Judge E. W. Clay in the 1870s. The Burbank Hills has numerous ATV trails and fossils. Geology The structural trend of rocks in the range is similar to rocks in the northern Mountain Home Range to the southwest and Conger Range and central Confusion Range to the northeast. These are chiefly Devonian to Permian carbonate rocks arranged in a massive syncline In structural geology, a syncline is a fold with younger layers closer to the center of the structure, whereas an anticline is the inverse of a syncline. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Home Range
The Mountain Home Range is a north-south trending mountain range in western Beaver County in southwest Utah, United States. It is part of the Basin and Range Province. It is bound by Hamlin Valley to the west, Snake Valley (part of this area known as Antelope Valley on some maps) to the north, Pine Valley to the east, and trends into the Indian Peak Range to the south. Collectively, the Mountain Home Range and Indian Peak Range are known as the Needle Mountains due to their jagged nature. The highest peak in the range, known simply as the 'Needle benchmark,' is tall. The range is very uncommonly used by humans, and is more known for wildlife and wild horses. Geology The northern part of the range is made of Paleozoic carbonate rocks which are part of a long structural trend of rocks that go through the Burbank Hills, Conger Range, and Confusion Range. This is highlighted by a massive (30 by 50 mile) syncline. The southern part of the range is made of mid-Tertiary ignimbrite ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Syncline
In structural geology, a syncline is a fold with younger layers closer to the center of the structure, whereas an anticline is the inverse of a syncline. A synclinorium (plural synclinoriums or synclinoria) is a large syncline with superimposed smaller folds. Synclines are typically a downward fold (synform), termed a synformal syncline (i.e. a trough), but synclines that point upwards can be found when strata have been overturned and folded (an antiformal syncline). Characteristics On a geologic map, synclines are recognized as a sequence of rock layers, with the youngest at the fold's center or ''hinge'' and with a reverse sequence of the same rock layers on the opposite side of the hinge. If the fold pattern is circular or elongate, the structure is a basin. Folds typically form during crustal deformation as the result of compression that accompanies orogenic mountain building. Notable examples * Powder River Basin, Wyoming, US * Sideling Hill roadcut along Interstate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carbonate Rock
Carbonate rocks are a class of sedimentary rocks composed primarily of carbonate minerals. The two major types are limestone, which is composed of calcite or aragonite (different crystal forms of CaCO3), and dolomite rock (also known as dolostone), which is composed of mineral dolomite (CaMg(CO3)2). Calcite can be either dissolved by groundwater or precipitated by groundwater, depending on several factors including the water temperature, pH, and dissolved ion concentrations. Calcite exhibits an unusual characteristic called retrograde solubility in which it becomes less soluble in water as the temperature increases. When conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together or it can fill fractures. Karst topography and caves develop in carbonate rocks because of their solubility in dilute acidic groundwater. Cooling groundwater or mixing of different groundwaters will also create conditions suitable for cave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian
The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the region of Perm in Russia. The Permian witnessed the diversification of the two groups of amniotes, the synapsids and the sauropsids ( reptiles). The world at the time was dominated by the supercontinent Pangaea, which had formed due to the collision of Euramerica and Gondwana during the Carboniferous. Pangaea was surrounded by the superocean Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditions, rose to dominance in place of their am ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Confusion Range
The Confusion Range is a north-south trending mountain range in west-central Utah, United States. It is bounded by Snake Valley to the west, Tule Valley to the east, the Great Salt Lake Desert to the north, and the Ferguson Desert to the south. The range trends into the Burbank Hills, Mountain Home Range, and the Wah Wah Mountains to the south. In the central part of the range, an offshoot of the mountains to the west is known as the Conger Range. The Confusion Range is named for its "rugged isolation and confusing topography."Van Cott, J. W., 1990, Utah Place Names, The highest peaks in the range are Conger Mountain , which is 7,713 feet tall, and King Top , which is 8,350 feet tall. The geology of the Confusion range is deformed Silurian to Permian limestones, dolomites, and shales.Chronic, Halka, 1990, Roadside Geology of Utah, There are three main ways to travel through the Confusion Range: *Around the north end, from Callao, Utah to Sand Pass *On old Highway 6/50, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conger Range (Utah)
The Conger Range, also called the Conger Mountains, is a mountain range in Quttinirpaaq National Park on Ellesmere Island, Nunavut, Canada, beginning about west of Mount Osborne. It is part of the Arctic Cordillera which is a vast dissected mountain system extending from Ellesmere Island to the northernmost tip of Labrador and northeastern Quebec. The Conger Range is a structural extension of the Garfield Range and continues into the highlands north of the head of Hare Fiord. The overall extent of the range is about . Most of its peaks are ice-covered, although nearly all of the southern slopes are ice-free. Many of the valleys between the peaks are filled with glacial tongues spilling out to the south from the Grand Land Ice Cap. Its highest point is Mount Biederbick at . The Conger Range was named by American Polar explorer Adolphus Greely Adolphus Washington Greely (March 27, 1844 – October 20, 1935) was a United States Army officer and polar explorer. He attained the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
All-terrain Vehicle
An all-terrain vehicle (ATV), also known as a light utility vehicle (LUV), a quad bike, or simply a quad, as defined by the American National Standards Institute (ANSI); is a vehicle that travels on low-pressure tires, with a seat that is straddled by the operator, along with handlebars for steering control. As the name implies, it is designed to handle a wider variety of terrain than most other vehicles. Although it is a street-legal vehicle in some countries, it is not street-legal within most states, territories and provinces of Australia, the United States or Canada. By the current ANSI definition, ATVs are intended for use by a single operator, although some companies have developed ATVs intended for use by the operator and one passenger. These ATVs are referred to as tandem ATVs. The rider sits on and operates these vehicles like a motorcycle, but the extra wheels give more stability at slower speeds. Although most are equipped with three or four wheels, six-wheel mode ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utah
Utah ( , ) is a state in the Mountain West subregion of the Western United States. Utah is a landlocked U.S. state bordered to its east by Colorado, to its northeast by Wyoming, to its north by Idaho, to its south by Arizona, and to its west by Nevada. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin. Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo and Ute. The Spanish were the first Europe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Burbank, Utah
Burbank is a small farming unincorporated community located on the western edge of Millard County, Utah, United States, just east of the Nevada border. It is located in the southern part of Snake Valley, near the opening (northern border) of Hamlin Valley. History It was founded as a Mormon farming community in the 1870s, with an early post office located at the Dearden Ranch. It was named after Margie Burbank Clay, the wife of local Judge E. W. Clay. Margie's obituary states that it was named in August 1949 after her mother when she, Margie, was age 96. Her mother was Laura Ann (Willard) Burbank (1819-1893). ''Clay'' was used as the name of the major spring that was first used by the settlers. This spring is the main source of water for Pruess Lake, to the north. Outlaws, cattle rustlers, and uncertainty over the local water sources caused the abandonment of the community, with the exception of the Dearden Ranch. The Dearden Ranch was started in 1886 and has been home t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antelope Valley (southwest Millard County, Utah)
The Antelope Valley of southwest Millard County, Utah, United States, is a small long valley, adjacent the Ferguson Desert and southwest of Sevier Lake. The valley is just east of the Nevada border, with Snake Valley and the Burbank Hills. The other Antelope Valley of Utah occurs east in the Great Basin, in southeast Emery County and extending into adjacent Wayne County. The Desert Biosphere Reserve forms the entire southeast, central & south valley border, where the small, low elevation arid Tunnel Springs Mountains are located.Utah Atlas & Gazetteer, p. 40. Description The Antelope Valley is southwest-northeast trending with a drainage northeast into the Ferguson Desert area. The valley also drains from the northeast flank of the Mountain Home Range adjacent the Nevada border to the southwest. The valley is narrow, only about , at its widest. Access Utah State Route 21 transects the upper region of the valley at the alluvial fans of the Mountain Home Range. Route 21 crossi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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