| Millions of years ago, the Gulf extended through the Salton basin to present day Indio. The river intersected the Gulf near what is now Yuma. As deposits of sediment built up in the former delta, a low 10-mile wide berm was created which extended 30 miles from Yuma to the Cocopah Mountains on the west side of the valley.
Eventually, the berm divided the north and south sides of the Gulf. The lake left to the north dried up. The Gulf to the south was pushed further and further south as segments continued to be deposited.
The river itself was fickle in where it flowed. Depending upon its sediment deposits, it would change course, flowing sometimes south around the large berm to the Gulf and sometimes north to the Salton Sea basin. Todays New and Alamo Rivers flow in former Colorado River water courses. For roughly the last million years, the river has changed course, leaving sediments on both sides of the berm and freshwater lakes behind in the Salton Sink.
Many people think that the Salton Sea is a man-made lake, says Salton Sea Authority Board Member, Corky Larson Over thousands of years the meandering Colorado River Delta created many Salton Seas. All these giant lakes were really natural phenomena, Larson added.
Over thousands of years the meandering Colorado River Delta created many Salton Seas.
Corky Larson,
Salton Sea Authority Board Member
In a December 2000 report, entitled An Inventory and Evacuation of Lake Cahuilla Cultural Resources along Imperial Irrigation Districts SA-Line, San Diego and Imperial Counties, authors Jerry Schaefer, Ph.D., RPA and Ken Moslak, Associate Archaeologist note that One of the most dynamic and dramatic aspects of the Colorado Desert paleoenvironment affecting human occupation was the flooding of the Salton Trough to form ancient Lake Cahuilla.
When the Salton basin filled completely, the lake was approximately six times the size of the current Salton Sea.
The Imperial and Coachella Valleys filled with water in about 18 years to form the largest fresh water lake in California. It was 110 miles long, and 32 miles wide, and over 280 feet deep at the center.The lake filled to an elevation of 40 ft above sea level, the height of the Colorado Delta that acted as a dam, according to the Schaefer report. It adds, Radiocarbon dates from marsh deposits and archaeological sites around the lake indicate three to four major lacustrine phases (periods when the lake was filled) over the last 2000 years, each lasting several hundred years.
In fact, while more research is needed, it is possible the river may have flowed north to the Salton basin more often than it did to the gulf over that time.
There were also partial infillings and many fluctuations in lake levels. Recent research has also demonstrated that there was at least a partial infilling as recently as A.D. 1600-1700 (Schaefer 1994, 2000 Laylander 1994, 1995), Schaefer writes.
A number of smaller lakes existed after 1600, including nine during the 1800s. Shoreline evidence of travertine deposits, mollusk and fish remains, vegetative evidence, and tribal sites document the history of the lakes.
The 2000 Schaefer report: Each time the lake filled, Indians from the Colorado River on the east and the Peninsular Range and desert fringes to the west established seasonal settlements along the sandy beaches of the shoreline
The lake provided abundant fish, a species of freshwater mollusk, migratory waterfowl, cattail, reeds, and other marsh vegetation especially on the western side of the lake, stone fish traps were constructed in the shallow waters to take advantage of natural fish behavior to hide in rocky enclosures when startled or during spawning. Today, parallel lines of these V-shaped stone traps can be seen from aerial photographs in the now dry desert where the prehistoric ancestors of the Cahuilla and Kumeyaay (Kamia) Indians fished and where they built new lines of traps as the lake waters receded.
The Schaeffer report notes that formation of Lake Cahuilla was so important that at least one Cahuilla lineage preserved the oral history of the event, describing how they were forced from the low basin by the rising waters. They later returned down to the shoreline to fish, gradually descending to lower elevations as the waters retreated..
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