Bridgeport Valley | |
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View of the Sierra Nevada from the floor of the Bridgeport Valley | |
Length | 10 mi (16 km) |
Width | 7.5 mi (12.1 km) |
Area | 45 sq mi (120 km2) |
Depth | 2,000 ft (610 m) |
Geography | |
Country | United States |
State | California |
Region | Mono County |
Population center | Bridgeport |
River | East Walker River |
The Bridgeport Valley is a large, fertile mountain basin between the eastern Sierra Nevada and the Bodie Hills of the U.S. state of California. The valley is 10 miles (16 km) long and 7.5 miles (12.1 km) wide, and is used primarily for ranching. The East Walker River is the main stream flowing through the Bridgeport Valley; tributaries include Robinson and Swauger Creeks. [1] The only town in the valley is Bridgeport, near Bridgeport Reservoir, which is formed by a dam that floods the northern end of the valley.
The Sierra Nevada is a mountain range in the Western United States, between the Central Valley of California and the Great Basin. The vast majority of the range lies in the state of California, although the Carson Range spur lies primarily in Nevada. The Sierra Nevada is part of the American Cordillera, a chain of mountain ranges that consists of an almost continuous sequence of such ranges that form the western "backbone" of North America, Central America, South America and Antarctica.
The Bodie Hills are a low mountain range in Mono County, California, in the United States. The Bodie Hills are between Bridgeport and the Nevada border, where they become the Bodie Mountains in Mineral County, Nevada. The Sierra Nevada lies to the west. The mining district and town of Bodie, California, is located in the Bodie Hills.
In the United States, a state is a constituent political entity, of which there are currently 50. Bound together in a political union, each state holds governmental jurisdiction over a separate and defined geographic territory and shares its sovereignty with the federal government. Due to this shared sovereignty, Americans are citizens both of the federal republic and of the state in which they reside. State citizenship and residency are flexible, and no government approval is required to move between states, except for persons restricted by certain types of court orders. Four states use the term commonwealth rather than state in their full official names.
Although the surrounding terrain is predominantly steep and rugged, the floor of the valley is generally flat and lies at an elevation of some 6,460 feet (1,970 m). Vertical relief on the sheer western side can be up to 3,000 feet (910 m), while on the eastern side, the slopes are more gradual, rising 1,500 to 2,500 feet (460 to 760 m) above the valley floor. Numerous peaks exceeding 10,000 feet (3,000 m) in height border the valley within a few miles on the west, south and east sides. The highest mountain that directly borders the valley is Mount Jackson, at 9,377 feet (2,858 m) above sea level.
U.S. Highway 395 bisects the valley, running from southeast to northwest. California State Route 182 also runs through the northern portion of the valley.
State Route 182 is a state highway in the U.S. state of California in Mono County. The route connects U.S. Route 395 in Bridgeport to State Route 338 at the Nevada state line via the East Walker River valley.
The north, west and southwest slopes of the valley border on the Humboldt-Toiyabe National Forest.
Bridgeport Valley is believed to be a triangular graben valley, bordered by geologic faults on almost all sides. The bedrock below the valley floor has dropped significantly below the level of the surrounding peaks, and streams flowing into it from the Sierra have deposited several hundred feet of sediments into it, creating the flat floor seen today. Thus a major portion of the valley floor actually lies on a large alluvial fan formed by Robinson Creek sediment deposits to the southwest, where the creek exits out of the mountains into the Bridgeport Valley. The channels of the alluvial fan branch out towards the north, northeast and east creating a highly fertile and well-watered grassy region. One of the valley's alternate names, "Big Meadows", likely originated from this quality.
In geology, a graben is a depressed block of the crust of a planet bordered by parallel faults.
In 1857, gold was discovered close to the Bridgeport Valley, starting the first major gold rush to the east of the Sierra Nevada in California. [2]
California is a U.S. state on the western coast of North America. Covering an area of 163,696 sq mi (423,970 km2), California is geographically diverse. The Sierra Nevada, the fertile farmlands of the Central Valley, and the arid Mojave Desert of the south are some of the major geographic features of this U.S. state. It is home to some of the world's most exceptional trees: the tallest, most massive, and oldest. It is also home to both the highest and lowest points in the 48 contiguous states. The state is generally divided into Northern and Southern California, although the boundary between the two is not well defined. San Francisco is decidedly a Northern California city and Los Angeles likewise a Southern California one, but areas in between do not often share their confidence in geographic identity. The US Geological Survey defines the geographic center of the state at a point near North Fork, California.
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Owens Valley is the now-arid valley of the Owens River in eastern California in the United States, to the east of the Sierra Nevada and west of the White Mountains and Inyo Mountains on the west edge of the Great Basin. The mountain peaks on either side reach above 14,000 feet (4,300 m) in elevation, while the floor of the Owens Valley is about 4,000 feet (1,200 m), making the valley one of the deepest in the United States. The Sierra Nevada casts the valley in a rain shadow, which makes Owens Valley "the Land of Little Rain." The bed of Owens Lake, now a predominantly dry endorheic alkali flat, sits on the southern end of the valley.
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