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Fremont Canyon (Utah)
Fremont Canyon is a stream and a deep valley or canyon that runs from its mouth at its confluence with Coyote Creek at the head of Fremont Wash in Iron County, Utah, eastward across the Tushar Mountains to its head at on the west side of Fremont Pass in Garfield County, Utah. The Canyon was named for John C. Frémont John Charles Frémont or Fremont (January 21, 1813July 13, 1890) was an American explorer, military officer, and politician. He was a U.S. Senator from California and was the first Republican nominee for president of the United States in 1856 .... References Landforms of Iron County, Utah Canyons and gorges of Garfield County, Utah Canyons and gorges of Utah {{Utah-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Confluence
In geography, a confluence (also: ''conflux'') occurs where two or more flowing bodies of water join to form a single channel. A confluence can occur in several configurations: at the point where a tributary joins a larger river (main stem); or where two streams meet to become the source of a river of a new name (such as the confluence of the Monongahela and Allegheny rivers at Pittsburgh, forming the Ohio); or where two separated channels of a river (forming a river island) rejoin at the downstream end. Scientific study of confluences Confluences are studied in a variety of sciences. Hydrology studies the characteristic flow patterns of confluences and how they give rise to patterns of erosion, bars, and scour pools. The water flows and their consequences are often studied with mathematical models. Confluences are relevant to the distribution of living organisms (i.e., ecology) as well; "the general pattern ownstream of confluencesof increasing stream flow and decreasing s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coyote Creek (Fremont Wash)
Coyote Creek may refer to: Streams *Coyote Creek (Calaveras County), California *Coyote Creek (Contra Costa County), California, a tributary of South San Ramon Creek *Coyote Creek (Marin County), California * Coyote Creek (Oat Creek tributary), California *Coyote Creek (Santa Clara County), California *Coyote Creek (San Mateo County), California *Coyote Creek (Yolo County), California *Coyote Creek (Ventura County), California * Coyote Creek (San Gabriel River), California *Coyote Creek (Borrego Sink), California *Coyote Creek (Long Tom River), Oregon Other *Coyote Creek Trail, San Jose California - part of the National Recreation Trail system *Coyote Creek bicycle path, Los Angeles County, California *Coyote Creek Bridge, Lane County, Oregon *Coyote Creek State Park, New Mexico * Trails of Yellowstone National Park includes a Coyote Creek Trail See also *Coyote Gulch (California) Coyote Gulch is a stream in San Francisco, California San Francisco (; Spanish for " Saint F ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fremont Wash
Fremont Wash sometimes called Fremont Canyon in its upper reach, is a stream and a valley in the north end of Parowan Valley, in Iron County, Utah. Its mouth lies at its confluence with Little Salt Lake at an elevation of 5,686 feet / 1,733 meters. Its head is found at , the mouth of Fremont Canyon, an elevation of 6,476 feet / 1,974 meters. History Fremont Wash was originally known as North Canyon Creek for the North Canyon from which it issued into the Parowan Valley at Muley Point. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iron County, Utah
Iron County is a county in southwestern Utah, United States. As of the 2010 United States Census, the population was 46,163. Its county seat is Parowan, and the largest city is Cedar City. The Cedar City, UT Micropolitan Statistical Area includes all of Iron County. History Evidence of Fremont culture habitation ranging from 750 to 1250 AD exists in present Iron County. Petroglyphs of differing periods were carved into the walls of Parowan Gap NW of Parowan. Paiutes roamed the Parowan Valley in the centuries before Euro-American exploration; their descendants are now represented by the Southern Paiute Indian Reservation, which is headquartered in Cedar City. The Domínguez–Escalante expedition traveled through the Iron County area on October 12, 1776. Fur trapper Jedediah Smith is the first recorded Anglo-American to pass through the area (1826). Settlement of the area began in 1851, when LDS President Brigham Young directed members from the northern colonies to move i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tushar Mountains
The Tushar Mountains are the third-highest mountain range in Utah after the Uinta Mountains and the La Sal Range. Located in the Fishlake National Forest, Delano Peak, 12,174 ft (3,711 m) NAVD 88, is the highest point in both Beaver and Piute counties and has a prominence of 4,689 ft (1,429 m). Delano Peak is named for Columbus Delano (1809–1896), Secretary of the Interior, during the Grant administration. The Tushars receive an ample amount of snow annually even though they are situated within the rainshadow of the Sierra Nevada range in California and the Snake Range located in Nevada. The main part of the range is in Beaver, Piute and Sevier counties. The northwestern corner extends into the southeastern corner of Millard County, and the southern end extends into the corners of Garfield and Iron counties. The Tushars are bounded roughly by I-15 to the west, I-70 to the north, US–89 to the east and U–20 to the south. U–153 crosses the southern part of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fremont Pass (Utah) – a pass separating the San Gabriel Mountains from the Santa Susana Mountains, once mistakenly known as "Fremont Pass"
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Fremont Pass may mean one of the following: Mountain passes *Fremont Pass (Colorado) – a pass on the Continental Divide of the Americas in Lake County, Colorado, United States *Fremont Pass (Nevada) – a pass in Washoe County, Nevada, United States * Fremont Pass (Utah) – a pass in Garfield County, Utah, United States *Newhall Pass - Beale's Cut Stagecoach Pass Beale's Cut Stagecoach Pass (also known as the Fremont Pass, San Fernando Pass, and the Newhall Cut) was a stagecoach pass built in 1859 in what is now Santa Clarita, California. The Pass was designated a California Historical Landmark (No. 1006 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Garfield County, Utah
Garfield County is a county in south central Utah, United States. As of the 2010 United States Census the population was 5,172, making it the fifth-least populous county in Utah; with about 0.98 inhabitants per square mile, it is also the least densely populated county in Utah. Its county seat and largest city is Panguitch. History The Utah Territory legislature created the county on March 9, 1882, with areas partitioned from Iron County. It was named for James A. Garfield, the twentieth President of the United States, who had died six months earlier. The border with Iron County was adjusted in 1884, and Garfield County's boundaries have remained intact since then. Geography The Colorado River, flowing southwestward through a deep gorge, forms the eastern boundary. The Dirty Devil River flows southward through the east end of the county to discharge into Colorado at the county's border. Westward, the cliffs of tributary canyons give way to the barren stretches of the San Rafa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John C
John is a common English name and surname: * John (given name) * John (surname) John may also refer to: New Testament Works * Gospel of John, a title often shortened to John * First Epistle of John, often shortened to 1 John * Second Epistle of John, often shortened to 2 John * Third Epistle of John, often shortened to 3 John People * John the Baptist (died c. AD 30), regarded as a prophet and the forerunner of Jesus Christ * John the Apostle (lived c. AD 30), one of the twelve apostles of Jesus * John the Evangelist, assigned author of the Fourth Gospel, once identified with the Apostle * John of Patmos, also known as John the Divine or John the Revelator, the author of the Book of Revelation, once identified with the Apostle * John the Presbyter, a figure either identified with or distinguished from the Apostle, the Evangelist and John of Patmos Other people with the given name Religious figures * John, father of Andrew the Apostle and Saint Peter * Pope Jo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Iron County, Utah
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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