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The last time that the Mojave River reached Lake Harper was between 25,000 and 20,000 years before present, [6] but this finding was later considered to be doubtful. [ 4 ] Harper Lake contained water and a natural marsh into the early 20th century when agricultural development began to deplete the groundwater that sustained its level.
In 1960, Metropolitan, along with 30 other public agencies, signed a long-term contract that made possible the construction of the State Water Project, including reservoirs, pumping plants and the 444-mile California Aqueduct (715 km), which serves urban and agricultural agencies from the San Francisco Bay to Southern California.
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]
Cima volcanic field is a volcanic field in San Bernardino County, California, close to the border with Nevada. [3] [4] The volcanic field covers a surface area of 600 km 2 (230 sq mi) within the Mojave National Preserve west of the Cima Dome and consists of about 40 volcanic cones with about 60 lava flows. The volcanic cones range from simple ...
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.
The Calico Early Man Site is an archaeological site in an ancient Pleistocene lake located near Barstow in San Bernardino County in the central Mojave Desert of Southern California. This site is on and in late middle- Pleistocene fanglomerates (now-cemented alluvial debris flow deposits) known variously as the Calico Hills, the Yermo Hills, or ...