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California Hollow (Beaver County, Utah)
California Hollow is a valley in the Black Mountains in Beaver and Iron County, Utah. Its mouth lies at an elevation of . It heads at , at an elevation of 6,940 feet, in Beaver County. History California Hollow lay along part of the original route of what was known during the California Gold Rush as the ''Southern Route'' of the California Trail, (later the Mormon Road), which passed over the Black Mountains between Greenville, Utah and Muley Point, on the way to California. In 1855 the Mormon Road was realigned eastward from this old route over the Black Mountains to one from a crossing at Beaver, Utah to Muley Point through more wagon friendly terrain in Nevershine Hollow and over Beaver Ridge into the canyon of 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. ... ... [...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] |
Beaver, Utah
Beaver is a city in, and county seat of, Beaver County in southwestern Utah, United States. The population was 3,112 at the 2010 census. History Indigenous peoples lived in this area for thousands of years, as shown by archeological evidence. A number of identified prehistoric sites have been found in Beaver County, dating to the Archaic and Sevier Fremont periods. A prehistoric obsidian quarry site has been identified in the nearby Mineral Mountains. The historic Southern Paiute inhabited the region well before encountering the first European explorers. The 1776 Dominguez–Escalante Expedition is the first known European exploration in this area. In 1847–1848, Mormons from the United States developed a trade route through the Beaver River valley between their new settlements at Salt Lake City in the Utah Territory and Los Angeles, which was still part of Alta California, Mexico. The original route crossed the river three miles downstream from Beaver at the site that ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of Utah
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] |
Valleys Of Iron County, Utah
A valley is an elongated low area often running between hills or 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 glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these 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 areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of Beaver County, Utah
A valley is an elongated low area often running between hills or 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 glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these 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 areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ... [...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] |
Beaver Ridge (Beaver County, Utah)
Beaver Ridge a ridge in Beaver County, Utah. It lies south of Nevershine Hollow and north of the canyon of Fremont Wash. It reaches an elevation of . History Beaver Ridge is the top of the pass between the valley of the Beaver River and the Parowan Valley. This was the apex of the 1855 cutoff from the original, more difficult route of the Mormon Road in the Black Mountains to the west. The 1855 cutoff made a crossing at Beaver, Utah, (3 miles east up the Beaver River from the old crossing at modern Greenville, Utah), passed through more wagon friendly terrain in Nevershine Hollow and over Beaver Ridge into the canyon of 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. ... to Muley Point.Edward Leo Lyman, Overland Journey from Utah to California: Wagon Travel from th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nevershine Hollow
Nevershine Hollow is a valley east of the South Hills, in Beaver County, Utah. The mouth of the valley is at an elevation of . Its head is at an elevation of 6,500 feet at , north of Beaver Ridge. History Nevershine Hollow was on the new 1855 cutoff route from the original Old Spanish Trail and the original and more difficult route of the Mormon Road in the Black Mountains to the west. The 1855 cutoff made a crossing at Beaver, Utah, (3 miles east up the Beaver River from the old crossing at modern Greenville, Utah), passed through more wagon friendly terrain in Nevershine Hollow and over Beaver Ridge into the canyon of 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. ... to Muley Point.Edward Leo Lyman, Overland Journey from Utah to California: Wagon Travel from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muley Point (Iron County, Utah)
Muley Point is a cliff in Iron County, Utah. It rises to an elevation of . It overlooks the northern end of the Parowan Valley, where 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 meter ... enters it. References Landforms of Iron County, Utah {{Utah-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black Mountains (Utah)
The Black Mountains is a long mountain range in northeastern Iron County and southeastern Beaver County in southwestern Utah, United States. The range borders the northeast portion of the Escalante Desert, and the range's southeast flank trends with the Hurricane Cliffs and Parowan Valley. In the south section, of a southwest trending ridgeline, is the Parowan Gap Petroglyphs Site. At the terminus of the ridgeline, the pass at the Summit, Utah region, there is the site of the Old Spanish National Historic Trail as it crossed into the northeast of Cedar Valley, the site of Cedar City. Interstate 15 (I-15) traverses the southeast region of the range from Cedar City, to Greenville-Beaver. Description The Black Mountains have a complex shape. It has an east-west ridgeline at the north perimeter with the Beaver River in the west, and Minersville Reservoir in the center; the northeast foothills border the region of Beaver-Greenville, Utah. The highpoint of the range, Mahogany Kno ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greenville, Utah
Greenville is an unincorporated community in eastern Beaver County, Utah, United States. Description The community lies along State Route 21 southwest of the city of Beaver (the county seat of Beaver County). Its elevation is . Although Greenville is unincorporated, it has a post office, with the ZIP code of 84731. History The location of Greenville was originally a camp on the north side of a ford on the Beaver River, along the Mormon Road until 1855. That year, the road was rerouted up river to the crossing at what later became Beaver Beavers are large, semiaquatic rodents in the genus ''Castor'' native to the temperate Northern Hemisphere. There are two extant species: the North American beaver (''Castor canadensis'') and the Eurasian beaver (''C. fiber''). Beavers ar .... Greenville was first settled in 1861. The community was named for the thick green grass which covered the original town site. See also References External links Populated place ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mormon Road
Mormon Road, also known to the 49ers as the Southern Route, of the California Trail in the Western United States, was a seasonal wagon road pioneered by a Mormon party from Salt Lake City, Utah led by Jefferson Hunt, that followed the route of Spanish explorers and the Old Spanish Trail across southwestern Utah, northwestern Arizona, southern Nevada and the Mojave Desert of California to Los Angeles in 1847. From 1855, it became a military and commercial wagon route between California and Utah, called the Los Angeles – Salt Lake Road. In later decades this route was variously called the "Old Mormon Road", the "Old Southern Road", or the "Immigrant Road" in California. In Utah, Arizona and Nevada it was known as the "California Road". Mormon Road 1847–1855 Jefferson Hunt and Mormon Veterans Expeditions 1847–1848 The wagon road later called the "Mormon Road" was pioneered by a Mormon party with pack horses, led by Jefferson Hunt, intent on obtaining supplies for the stru ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
