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Encyclopedia > Lake Cahuilla

Prehistoric Lake Cahuilla (also known as Lake LeConte and Blake Sea) was an extensive freshwater lake that filled the Coachella, Imperial, and Mexicali valleys of southeastern California and northeastern Baja California during the centuries prior to Spanish entry into the region. The Salton Sea (about 55 kilometers long, 25 kilometers wide, and at an elevation of 65 meters below sea level), which was accidentally created in 1905, is a much smaller analog of its prehistoric predecessor, Lake Cahuilla (about 180 kilometers long, 50 kilometers wide, and rising to 12 meters above sea level, drowning the present sites of the cities of Mexicali, El Centro, and Indio). The Salton Sea (with local/regional cities) The Salton Sea is an inland saline lake, located in the Colorado Desert in Southern California, north of the Imperial Valley. ...


Lake Cahuilla was created when the lower Colorado River shifted its course within its delta. Instead of flowing directly south to the head of the Gulf of California, the river's waters were diverted northwest into the Salton Basin, the base of which lay about 80 meters below sea level. Under climatic conditions similar to those of the early twentieth century, it would have taken about two decades of uninterrupted river flow to fill the basin to 12 meters above sea level (D. Weide 1976; Wilke 1978; Waters 1983; Laylander 1997). At that point, the lake would have overflowed to the south, feeding half of its waters through the Rio Hardy to the Gulf but losing the other half through evaporation. When the river shifted its course back to the south, the isolated basin would have taken more than five decades to completely dry out again.


The former presence of a large lake in the Salton Basin was remembered by the region's historic-period native inhabitants, the Cahuilla and the Kumeyaay (Wilke 1978; Laylander 2004). By the mid-nineteenth century, Euro-American visitors, including the geologist William P. Blake (1858), had recognized the lake's traces, including tufa deposits along the maximum shoreline, beaches, and deposits of freshwater mollusk shells. The Cahuilla are a group of Native Americans that have inhabited California for more than 2000 years, originally covering an area of about 2,400 square miles (6,200 km²). Evidence shows that when the Cahuilla first moved into the area a large body of water now called Lake Cahuilla... The Kumeyaay, also known as the Diegueño and sometimes confused with the Luiseño, are a Native American people of the extreme southwestern United States and northwest Mexico. ...


Malcolm J. Rogers (1945), a pioneering archaeology in the region, examined aboriginal pottery left on shoreline sites and concluded that the lake had been present between about A.D. 1000 and 1500. Subsequent studies have established that there were not one but several different high stands of the lake, both prior to A.D. 1000 and subsequent to 1500, including a stand as late as the seventeenth century, when Spanish explorers had already reached the lower Colorado River although not entering the Salton Basin (Wilke 1978; Waters 1983; Laylander 1997; Love and Dahdul 2002).


Native peoples harvested a range of resources associated with Lake Cahuilla in the otherwise-parched Colorado Desert. Prominent were freshwater fish (primarily bonytail - Gila elegans - and razorback sucker - Xyrauchen texanus), freshwater mollusks (Anodonta dejecta), water birds (particularly American coot - Fulica americana), and marsh plants (cattail - Typha, tule - Scirpus, and reed - Phragmites). Researchers have disagreed as to how important the role of Lake Cahuilla resources was within native subsistence strategies, and consequently how dramatically the lake's rises and falls shaped the region's late prehistory. Some have envisioned many permanent or semi-permanent settlements on the shores, producing severe regional upheavals when their supporting resources disappeared, while other researchers have seen the lake as only a marginal area within stable regional subsistence patterns (e.g., Aschmann 1959; M. Weide 1976; Wilke 1978; Schaefer 1994; Laylander 2006).



References


Aschmann, Homer. 1959. The Evolution of a Wild Landscape and Its Persistence in Southern California. Annals of the Association of American Geographers 49(3):34-57.


Blake, William Phipps. 1858. Report of a Geological Reconnaissance in California Made in Connection with the Ejxpedition to Survey Routes for a Railroad from the Mississippi River to the Pacific Ocean, under the Command of Lietu. R. S. Williamson, Corps Top. Eng'rs, in 1853. H. Baillière, New York.


Laylander, Don. 1997. "The Last Days of Lake Cahuilla: The Elmore Site". Pacific Coast Archaeological Society Quarterly 33(1-2):1-138.


Laylander, Don. 2004. "Remembering Lake Cahuilla". In The Human Journey & Ancient Life in California's Deserts: Proceedings from the 2001 Millennium Conference, edited by Mark W. Allen and Judyth Reed, pp. 167-171. Maturango Museum, Ridgecrest, California.


Laylander, Don. 2006. "The Regional Consequences of Lake Cahuilla". San Diego State University Occasional Archaeology Papers 1:59-77.


Love, Bruce, and Mariam Dahdul. 2002. "Desert Chronologies and the Archaic Period in the Coachella Valley". Pacific Coast Archaeological Society Quarterly 38(1-2).


Rogers, Malcolm J. 1945. "An Outline of Yuman Prehistory". Southwestern Journal of Anthropology 1:167-198.


Schaefer, Jerry. 1994. "The Challenge of Archaeological Research in the Colorado Desert: Recent Approaches and Discoveries". Journal of California and Great Basin Anthropology 16:60-80.


Waters, Michael R. 1983. "Late Holocene Lacustrine Chronology and Archaeology of Ancient Lake Cahuilla, California". Quaternary Research 19:373-387.


Weide, David L. 1976. "Regional Environmental History of the Yuha Desert". In Background to Prehistory of the Yuha Desert Region, edited by Philip J. Wilke, pp. 9-20. Ballena Press, Ramona, California.


Weide, Margaret L. 1976. "A Cultural Sequence for the Yuha Desert". In Background to Prehistory of the Yuha Desert Region, edited by Philip J. Wilke, pp. 81-94. Ballena Press, Ramona, California.


Wilke, Philip J. 1978. Late Prehistoric Human Ecology at Lake Cahuilla, Coachella Valley, California. Contributions of the University of California Archaeological Research Facility No. 38. Berkeley.


  Results from FactBites:
 
Ancient Lake Cahuilla (1492 words)
The last of the Pleistocene lakes to occupy the basin was Lake Cahuilla, identified on older maps as Lake Leconte.
Lake Cahuilla was possibly one of the largest lakes of the past.
The lake was almost 100 miles long by 35 miles across at its widest point, extending from the delta in Mexico north to the vicinity of Indio.
SDNHM: Paleontology Department (476 words)
Lake Cahuilla (also called Lake LeConte) was a former freshwater lake that periodically occupied a major portion of the Salton Trough during the Holocene, approximately 10,000 to 240 years ago.
Regardless of the exact timing of inundation, the former shoreline marking the maximum high stand for Lake Cahuilla is well-preserved around the margins of the Imperial Valley at an elevation of approximately 40 to 48 feet above sea level.
Filling of Lake Cahuilla occurred several times during the Holocene, and each time the filling was the result of natural diversion of the Colorado River from its delta in the Gulf of California to the, below-sea-level Salton Trough.
  More results at FactBites »


 

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