Bridgeport Valley

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Bridgeport Valley
Sierra Nevada near Bridgeport, California-1000px.jpeg
View of the Sierra Nevada from the floor of the Bridgeport Valley
Length10 mi (16 km)
Width7.5 mi (12.1 km)
Area45 sq mi (120 km2)
Depth2,000 ft (610 m)
Geography
CountryUnited States
StateCalifornia
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.

Sierra Nevada (U.S.) mountain range

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.

Bodie Hills

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.

U.S. state constituent political entity of the United States

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.

California State Route 182 highway in California

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.

Graben Depressed block of planetary crust bordered by parallel faults

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]

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References

  1. "Bridgeport Valley Groundwater Basin" (PDF). California's Groundwater Bulletin 118. California Department of Water Resources. Retrieved 2011-01-06.
  2. Hough, Susan Elizabeth (2004). Finding faults in California: an earthquake tourist's guide. Mountain Press Publishing. p. 193. ISBN   0-87842-495-4.