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Mono and Lake
Relief map of Mono Lake and surrounding area, including nearby Lake Tahoe and Yosemite National Park ( area within yellow boundaries ); California-Nevada state border shown
Mono Lake ( ) is a large, shallow saline soda lake in Mono County, California, formed at least 760, 000 years ago as a terminal lake in a basin that has no outlet to the ocean.
The human history of Mono Lake is associated with its productive ecosystem.
The Mono Lake Committee formed in response, winning a legal battle that forced Los Angeles to partially restore the lake level.
USGS map of the Mono Lake area, showing geological features
The tributaries of Mono Lake include Lee Vining Creek, Rush Creek and Mill Creek which flows through Lundy Canyon.
This activity was northwest of Mono Basin and included the formation of Aurora Crater, Beauty Peak, Cedar Hill ( later an island in the highest stands of Mono Lake ), and Mount Hicks.
Mono Lake is believed to have formed at least 760, 000 years ago, dating back to the Long Valley eruption.
Sediments located below the ash layer hint that Mono Lake could be a remnant of a larger and older lake that once covered a large part of Nevada and Utah, which would put it among the oldest lakes in North America.
Currently, Mono Lake is in a geologically active area at the north end of the Mono – Inyo Craters volcanic chain and is close to Long Valley Caldera.
Volcanic activity continues in the Mono Lake vicinity: the most recent eruption occurred 350 years ago, resulting in the formation of Paoha Island.
Lakeside of Mono Lake, 1999
An important, and unintentional, consequence of ending the water diversions was the onset of a period of " meromixis " in Mono Lake.
In the time prior to this, Mono Lake was typically " monomictic "; which means that at least once each year the deeper waters and the shallower waters of the lake mixed thoroughly, thus bringing oxygen and other nutrients to the deep waters.
Mono Lake has experienced meromictic periods in the past ; this most recent episode of meromixis, brought on by the end of the water diversions, commenced in 1994 and had ended by 2004.
Mono Lake alkali flies
The lake is famous for the Mono Lake brine shrimp, Artemia monica, a tiny species of brine shrimp, no bigger than a thumbnail, that are endemic.
Mono Lake is a vital resting and eating stop for migratory shorebirds and has been recognized as a site of international importance by the Western Hemisphere Shorebird Reserve Network.
Nearly 2, 000, 000 waterbirds, including 35 species of shorebirds, use Mono Lake to rest and eat for at least part of the year.

Mono and formed
Inyo County was formed in 1866 from the territory of the unorganized Coso County created on April 4, 1864 from parts of Mono and Tulare Counties.
Mono County was formed in 1861 from parts of Calaveras County, Fresno County and Mariposa County.
In 1978, the Mono Lake Committee was formed to protect Mono Lake.
A project called Mono. XNA was formed to port XNA to the open source and cross-platform Mono framework.
From the codebase of Mono. XNA and SilverSprite a new project called MonoGame was formed to port XNA to several mobile devices.

Mono and because
Despite there being trillions of these creatures in Mono Lake, it was felt that rising levels of salinity and sodium hydroxide concentration of the lake would endanger them because of the increase in pH.
Little is known about Mono other than that she was somehow sacrificed because she was believed to have a cursed destiny.

Mono and lies
It lies along the Sierra Crest that divides Fresno County from Mono County, California.
It lies in Mono County, California, between McGee Canyon and Hilton Lakes.
The main difference lies in the Havok physics engine, which is used for the Mono system.

Mono and Basin
Five million years ago, the Sierra Nevada was an eroded set of rolling hills and Mono Basin and Owens Valley did not yet exist.
From 4. 5 to 2. 6 million years ago, large volumes of basalt were erupted around what is now Cowtrack Mountain ( east and south of Mono Basin ); eventually covering and reaching a maximum thickness of.
* Roadside Geology and Mining History of the Owens Valley and Mono Basin
One notable feature of the Basin and Range is Mono Lake, which is the oldest lake in North America.
In 1941 the Los Angeles Department of Water and Power extended the Los Angeles Aqueduct system further upriver into the Mono Basin.
The Mono Basin population of Sage Grouse may also be distinct.
LADWP started buying water rights in the Mono Basin ( the next basin to the north of the Owens Valley ).
* The Mono Basin Project DWP
* Mono Basin National Scenic Area
Russell glacier and Mount Russell in Alaska as well as Mount Rainier's Russell Glacier and the prehistoric Lake Russell in California's Mono Basin are also named for him.
Mount Lyell divides the Tuolumne River watershed to the north, the Merced to the west, and the Rush Creek drainage in the Mono Lake Basin to the southeast.
The Mono () are a Native American people who traditionally live in the central Sierra Nevada Mountains, the Eastern Sierra ( generally south of Bridgeport ), the Mono Basin, and adjacent areas of the Great Basin.
In 1984 the Federal Government designated surrounding lands as the Mono Basin National Forest Scenic Area.
* official Mono Basin National Forest Scenic Area website

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