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Minnesota Geological Survey via Minnesota Geologic Topics; select Bedrock Geology, then select Geologic Map of Minnesota's Bedrock Geology: Author: Mark A. Jirsa, Terrence J. Boerboom, V.W. Chandler, John H. Mossler, Anthony C. Runkel, and Dale R. Setterholm: Permission (Reusing this file)
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Lake Mojave is an ancient former lake fed by the Mojave River that, through the Holocene, occupied the Silver Lake and Soda Lake basins in the Mojave Desert of San Bernardino County, California. Its outlet may have ultimately emptied into the Colorado River north of Blythe .
The Deep Creek drainage basin is 135 square miles (350 km 2) in size. [2] Most of the drainage basin is located in the San Bernardino National Forest . For most of its length it is a remote, swift-flowing mountain stream, with a riverbed characterized by "deep pools and boulder strewn reaches". [ 11 ]
Coyote Dry Lake is a dry lake bed in the Mojave Desert of San Bernardino County, California, 15 mi (24 km) northeast of Barstow. The lake is approximately 10 km (6.2 mi) by 6 km (3.7 mi) at its widest point. Coyote Dry Lake lies to the south of Fort Irwin Military Reservation and southwest of the Tiefort Mountains. St.
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It formerly was the Mojave River's terminal lake, [5] and received about 1 millimetre per year (0.039 in/year) of sediment. [45] The Coyote Basin was not permanently coupled to the main lake body; its relatively large surface area and consequently high evaporation would have stabilized lake levels when it was connected to Lake Manix proper. [46]
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.