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About: Lake Cahuilla     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatFormerLakes, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: Thingplacedbo:Locationschema:BodyOfWaterschema:Placenatural placeyago:WikicatLakesOfTheGreatBasinyago:BodyOfWater109225146yago:Lake109328904yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntitybody of waterlakeyago:Thing100002452yago:WikicatFormerLakes New Facet based on Instances of this Class

Lake Cahuilla (/kəˈwiː.ə/ kə-WEE-ə; also known as Lake LeConte and Blake Sea) was a prehistoric lake in California and northern Mexico. Located in the Coachella and Imperial Valleys, it covered surface areas of 5,700 km2 (2,200 sq mi) to a height of 12 m (39 ft) above sea level during the Holocene. During earlier stages of the Pleistocene, the lake reached even higher elevations, up to 31–52 m (102–171 ft) above sea level. During the Holocene most of the water came from the Colorado River with little contribution from local runoff; in the Pleistocene local runoff was higher and it is possible that Lake Cahuilla was supported solely from local water sources during the Wisconsin glaciation. The lake overflowed close to Cerro Prieto into the Rio Hardy, eventually draining into the Gulf of Cal