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Pine Valley (Beaver, Millard, Iron Counties, Utah)
Pine Valley is a long valley in southwestern Utah, United States. Most of the valley lies in western Beaver and Millard counties; the extreme south of the valley arises in two mountain range regions in northwestern Iron County. The valley is endorheic, with a north-flowing Pine Valley Wash that ends in sinks. At about seven miles north of the sinks region, in a north valley area, lies the Pine Valley Hardpan, about long, east-west. The northwest of Pine Valley contains a long Desert Biosphere Reserve and Experimental Station. The southern stretch of the Tunnel Springs Mountains is in the experimental station. Description Pine Valley is about a long valley. The valley narrows in the south to about wide, where Pine Valley Wash originates. The valley is a north-south valley, but the southern turns southeasterly, paralleling a mountain ridgeline stretch of the Indian Springs Range bordered to the west. The south terminus of Pine Valley is at the merge point of the southeast ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wah Wah Mountains
The Wah Wah Mountains are a north-south trending range in west-central Utah, part of the larger Basin and Range Province. It is bounded by Pine Valley to the west, Wah Wah Valley to the east, the Escalante Desert to the south, and on trend with the Confusion Range to the north. The Wah Wah Mountains are located in Beaver and Millard counties. State Route 21 bisects the range, crossing over Wah Wah Summit at about above sea level. Elevations range from about at the mountain front to in the southern Wah Wahs. The "Wah Wah" name comes from Wah Wah Springs, on the eastern slope of the mountain range. "Wah Wah" is reported to mean "good clear water". The Bureau of Land Management, which administers most of the land within the Wah Wah Mountains, has designated two wilderness study areas, one in the north and one in the central portion of the range. Geology The Wah Wah Mountains are made up of Neoproterozoic- to Paleozoic-aged sedimentary rocks (limestone, dolomite, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Indian Springs Range
Indian or Indians may refer to: Peoples South Asia * Indian people, people of Indian nationality, or people who have an Indian ancestor ** Non-resident Indian, a citizen of India who has temporarily emigrated to another country * South Asian ethnic groups, referring to people of the Indian subcontinent, as well as the greater South Asia region prior to the 1947 partition of India * Anglo-Indians, people with mixed Indian and British ancestry, or people of British descent born or living in the Indian subcontinent * East Indians, a Christian community in India Europe * British Indians, British people of Indian origin The Americas * Indo-Canadians, Canadian people of Indian origin * Indian Americans, American people of Indian origin * Indigenous peoples of the Americas, the pre-Columbian inhabitants of the Americas and their descendants ** Plains Indians, the common name for the Native Americans who lived on the Great Plains of North America ** Native Americans in the ... [...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 Millard 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. ... [...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] |
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] |
List Of Valleys Of Utah
This is a list of valleys of Utah. Valleys are ordered alphabetically by county and then for the entire state. Beaver County * Beaver Valley (Utah) * Hamlin Valley * Milford Valley * Pine Valley (Beaver, Millard, Iron counties, Utah) (in Beaver, north Iron, and south Millard counties) * Wah Wah Valley Box Elder County * Bear River Valley * Blue Creek Valley * Curlew Valley * Junction Valley * Upper Raft River Valley Cache County * Ant Valley * Cache Valley Carbon County * Castle Valley (Carbon, Emery, and Sevier counties, Utah) * Emma Park * Whitmore Park Daggett County * Lucerne Valley Davis County * Salt Lake Valley Duchesne County * Pleasant Valley * Roosevelt Valley Emery County * Antelope Valley (Wayne-Emery counties, Utah) * Castle Valley (Carbon, Emery, and Sevier counties, Utah) * Gunnison Valley (Emery and Grand counties, Utah) * Joe's Valley * San Rafael Valley Garfield County * Bear Valley Junction, Utah * Circle Valley' * Johns Valley ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Milford, Utah
Milford is a city in Beaver County, Utah, United States. The population was 1,409 at the 2010 census and 1,394 as of a 2019 Census Bureau estimate. History Although settlers had established ranches in the area in the 1870s, Milford was not developed until after construction of the San Pedro, Los Angeles and Salt Lake Railroad in 1880, which established a station here. Milford is a constructed name, an abbreviated form of mill and ford. During the Great Depression, workers from a nearby Civilian Conservation Corps camp constructed a road from Milford to Beaver, to improve connections. Milford Flat Wildfire Lightning caused a massive wildfire to start near Milford at 3:45 p.m. Friday, July 6, 2007. On July 8 the fire was declared the largest in Utah's history, having burned more than . Demographics As of the 2000 census, there were 1,451 people, 484 households, and 357 families residing in the city. The population density was 753.7 people per square mile (290.3/km2). ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Garrison, Utah
Garrison is an unincorporated community in western Millard County, Utah, United States. It is home to a Utah Department of Transportation yard and office, but other than that, offers no services. ZIP code The 84728 ZIP code, which includes Garrison as the primary population center, has 158 residents spread out over 335.54 square miles. The median household income is $37,857 and 62 out of 83 housing units are occupied. Three public school run by the Millard School District serve the area covered by the ZIP code: the Garrison School (elementary), Garrison 7th & 8th, and Eskdale High School. Geography Garrison is located in Snake Valley in the far west central area of the state just east of the Nevada state line. In fact, some of the town's farms and structures are legally in Nevada. The Great Basin National Park is in Nevada just a few miles west of the border, accessed via Baker. History Founded as a cattle rustling and outlaw community in the 1850s, the town of Garris ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Utah State Route 21
State Route 21 (SR-21) is a state highway in western Utah, running for in Millard and Beaver Counties from the Nevada state line near Garrison to Beaver. Route description SR-21 begins at the Nevada state line as a continuation of Nevada State Route 487 and heads southeast through Garrison. It continues southeast past Pruess Lake and continues through Mormon Gap and Halfway Summit. It turns east around Lime Point into Corral Canyon and over Wah Wah Summit. It then heads southeast between Grampian Hill and Squaw Peak into Squaw Gulch, where it turns northeast over Frisco Summit and east through the ghost town of Frisco. It then turns southeast and continues to Milford. SR-21 leaves Milford heading southeast across an agricultural area to Minersville. In Minersville, it turns east past Yellow Mountain, then turns northeast past Minersville Lake State Park. It continues through Adamsville, then turns east around Little Bald Hill through Greenville into Beaver. In Bea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lund, Utah
Lund is an unincorporated village located in the Escalante Valley of northwestern Iron County, Utah, United States, approximately northwest of Cedar City. The town, established in the early twentieth century, was a station stop on the Los Angeles and Salt Lake Railroad (later Union Pacific Railroad), and was a community center for early twentieth century homesteaders. The area's population was never large, however, and most early settlers were unsuccessful due to the region's harsh and arid climate. History Settlement activity in the Lund area began with the completion of the railway line through the Escalante Valley in the winter of 1898–99, but Lund's population remained extremely small until 1911, when the valley was opened to homestead settlement. The Lund townsite was platted in 1913, beginning a decade of relative activity at the location. The town was named for Robert C. Lund, who was a Utah State legislator, local mine owner, and a director of the Union Pacific R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
