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There are two water resource basin subdivisions of the Northern Mojave–Mono Lake subregion (HUC 1809). Northern Mojave–Mono Lake water resource subregion (HUC 1809) is one of 10 water resource subregions within the California water resource region and is one of 222 water resource subregions in the federally organized United States hydrologic unit system.
A freshwater lake developed in the basin about 400,000 – 500,000 years ago near the Calico Archaeological Site. The lake was present until the late Pleistocene. The last high stand of Lake Manix was at 543 m (1,781 ft) and had a surface area of approximately 236 km 2 (91 sq mi). This lake drained, probably catastrophically, approximately ...
Drainage basins include the Antelope Valley watershed, the Mojave watershed, Mono Basin, the Owens River watershed, and the Amargosa River watershed. [3] There are 77 state-recognized alluvial groundwater basins and subbasins in the South Lahontan hydrologic region, underlying approximately 55 percent of the land area. [2]
Lake Mojave in relation to other Pleistocene-era lakes in the region. The Mojave River is the principal river reaching the Lake Mojave basin, [3] and the principal river of the Mojave Desert. [5] Presently, a number of springs on the western side of the Lake Mojave basin form small waterbodies. [5]
The Manix, Mojave, and the Little Mojave lakes are all large but shallow. [ 13 ] : 7 Soda Lake is the principal saline basin of the Mojave Desert. Natural springs are typically rare throughout the Mojave Desert, [ 13 ] : 19 but there are two notable springs, Ash Meadows and Oasis Valley .
The latter basin is heavily dissected in comparison to the others. [7] These basins were at various points separated from each other by sills. [8] In the older history of the lake another basin named Cady Basin existed, before the Mojave River eroded through the Buwalda Ridge and connected it to the Afton Basin.
The Mojave River is an intermittent river in the eastern San Bernardino Mountains and the Mojave Desert in San Bernardino County, California, United States. Most of its flow is underground, while its surface channels remain dry most of the time, except for the headwaters and several bedrock gorges in the lower reaches.
Soda Lake (or Soda Dry Lake) is a dry lake at the terminus of the Mojave River [1] in the Mojave Desert of San Bernardino County, California. The lake has standing water during wet periods, and water can be found beneath the surface. Soda Lake along with Silver Lake are what remains of the large, perennial, Holocene Lake Mojave.