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The Bishop Tuff is a welded tuff which formed 764,800 ± 600 years ago as a rhyolitic pyroclastic flow during the approximately six-day eruption that formed the Long Valley Caldera. [1] [2] [3] Large outcrops of the tuff are located in Inyo and Mono Counties, California, United States. Approximately 200 cubic kilometers of ash and tuff erupted ...
Layers of the Bishop tuff, in a rock quarry in Chalfant Valley, about 25 km (16 mi) southwest of the Long Valley Caldera, laid down in phases of a major eruption 760,000 years ago. The known volcanic history of Long Valley Caldera area started a few million years ago when magma began to collect several miles below the surface.
Rock climbing in the Owens River Gorge. The Owens River Gorge is a steep 10 mi (16 km) canyon on the upper Owens River in eastern California in the United StatesThe canyon is located at the eastern edge of the Sierra Nevada mountains in southern Mono County, along the stretch of the river where it exits the Long Valley near its source and enters the north end of Owens Valley.
Bishop (formerly Bishop Creek) [5] is the most populous and only incorporated city in Inyo County, California, United States. It is located near the northern end of the Owens Valley within the Mojave Desert , at an elevation of 4,150 feet (1,260 m). [ 4 ]
Crowley Lake is a reservoir on the upper Owens River in southern Mono County, California, in the United States.Crowley Lake is 15 mi (24 km) south of Mammoth Lakes.. The lake was created in 1941 by the building of the Long Valley Dam by the Los Angeles Department of Water and Power (DWP), as storage for the Los Angeles Aqueduct and for flood control.
Robert Sibley Volcanic Regional Preserve is located in the Oakland Hills of the East Bay region of the San Francisco Bay Area, California. [1] The park is part of the East Bay Regional Parks District (EBRPD), covers 928 acres (3.76 km 2), and lies east of Oakland, partly in Alameda County and partly in Contra Costa County.
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The Lava Creek Tuff of Yellowstone Caldera and the Bishop Tuff of the Long Valley Caldera were deposited in the Corcoran Clay. [11] Before Lake Corcoran formed, the Central Valley was a bay open to the south via a passage, until 2 million years ago when the bay was separated from the ocean, probably due to northwestward movement of the Coast ...
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