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The Mono Basin is an endorheic drainage basin located east of Yosemite National Park in California and Nevada. [ 3 ] [ 4 ] It is bordered to the west by the Sierra Nevada , to the east by the Cowtrack Mountains , to the north by the Bodie Hills , and to the south by the north ridge of the Long Valley Caldera .
The current tribal name "Mono" is a Yokutsan loanword from the tribe's western neighbors, the Yokuts, who however hereby designated the Owens valley Paiutes as the southernmost Northern Paiute band living around "owens lake" / Mono Lake as monachie/monoache ("fly people") because fly larvae was their chief food staple and trading article [4 ...
Mono Basin History Museum: Lee Vining: Mono: High Sierra: Local history: website, operated by the Mono County Historical Society, located in a historic schoolhouse, Native American artifacts, gold mining implements, local history and culture, Nellie Bly's legendary Upside-Down House, farming and mining equipment
The Mono Basin National Forest Scenic Area Visitor Center is located 1/2 mile north of the town of Lee Vining, California, just east of Tioga Pass (the eastern entrance to Yosemite National Park), on U.S. Route 395. A variety of activities and exhibits introduce the natural and human history of the Mono Basin.
Mono traditional narratives include myths, legends, tales, and oral histories preserved by the Mono people, including the Owens Valley Paiute east of the Sierra Nevada and the Monache on that range's western slope, in present-day eastern California. An interesting contrast exists in Mono oral literature.
Present-day Mono Lake 38°00′N 119°00′W / 38.000°N 119.000°W / 38.000; -119.000 [ 1 ] Lake Russell is a former lake stage of Mono It was named in honour of Israel Russell , but is also known as Lake Mono in contrast to the present-day lake. [ 2 ]
Mono Lake Tufa State Natural Reserve is located near Yosemite National Park within Mono County, in eastern California. It was established in 1981 [ 2 ] by the California State Legislature to preserve the natural limestone " tufa tower " formations at Mono Lake .
The results of the litigation culminated with a SWRCB decision to restore fishery protection (stream) flows to specified minimums, and raise Mono Lake to 6,391 feet (1,948 m) above sea level. The agreement limited further exports from the Mono Basin to 16,000 acre⋅ft (19.7 million m 3) or less per year during the transition period. [31]