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Salton Sea - Wikipedia. Salton Sea. Location. Watch Andron Online Full Movie. Colorado Desert. Imperial and Riverside Counties, California, U. S. Coordinates. 33°1.

N1. 15°4. 8′W / 3. N 1. 15. 8°W / 3. Coordinates: 3. 3°1. N1. 15°4. 8′W / 3. N 1. 15. 8°W / 3.

Type. Endorheicrift lake. Primary inflows. Alamo River. New River. Whitewater River. Primary outflows.

None. Catchment area. Basin countries. United States, Mexico. Surface area. 34.

Max. depth. 43 ft (1. Water volume. 6,0.

Surface elevation−2. Settlements. Bombay Beach, Desert Beach, Desert Shores, Salton City, Salton Sea Beach, North Shore. References. U. S. Geological Survey Geographic Names Information System: Salton Sea. Map of the Salton Sea drainage area. The Salton Sea is a shallow, saline, endorheicrift lake located directly on the San Andreas Fault, predominantly in California's Imperial and Coachella Valleys. The lake occupies the lowest elevations of the Salton Sink in the Colorado Desert of Imperial and Riverside Counties in Southern California.

Its surface is 2. February 5, 2. 01. The deepest point of the sea is 5 ft (1. Death Valley. The sea is fed by the New, Whitewater, and Alamo Rivers, as well as agricultural runoff, drainage systems, and creeks. Over millions of years, the Colorado River has flowed into the Imperial Valley and deposited soil (creating fertile farmland), building up the terrain and constantly changing the course of the river.

For thousands of years, the river has flowed into and out of the valley alternately, creating a freshwater lake, an increasingly saline lake, and a dry desert basin, depending on river flows and the balance between inflow and evaporative loss. The cycle of filling has been about every 4. The latest natural cycle occurred around 1. Native Americans who talked with the first European settlers.

Fish traps still exist at many locations, and the Native Americans evidently moved the traps depending upon the cycle. The most recent inflow of water from the now heavily controlled Colorado River was accidentally created by the engineers of the California Development Company in 1.

In an effort to increase water flow into the area for farming, irrigation canals were dug from the Colorado River into the valley. Due to fears of silt buildup, a cut was made in the bank of the Colorado River to further increase the water flow. The resulting outflow overwhelmed the engineered canal, and the river flowed into the Salton Basin for two years, filling the historic dry lake bed and creating the modern sea, before repairs were completed.[2]While it varies in dimensions and area with fluctuations in agricultural runoff and rainfall, the Salton Sea is about 1. With an estimated surface area of 3. Salton Sea is the largest lake in California.[3][4] The average annual inflow is less than 1,2. However, due to changes in water apportionments agreed upon for the Colorado River under the Quantification Settlement Agreement of 2.

The lake's salinity, about 5. Pacific Ocean (3. Great Salt Lake (which ranges from 5. Recently, the concentration has been increasing at a rate of about 3% per year.[6] About 4,0. History[edit]The area was once part of a vast inland sea that covered a large area of Southern California. Geologists estimate that for three million years, at least through all the years of the Pleistocene glacial age, a large delta was deposited by the Colorado River in the southern region of the Imperial Valley.

Eventually, the delta reached the western shore of the Gulf of California, creating a barrier that separated the area of the Salton Sea from the northern reaches of the Gulf. Were it not for this barrier the entire Salton Sink along with the Imperial Valley would be submerged as the Gulf would extend as far north as Indio.[8]Since the exclusion of the ocean, the Salton Basin has over the ages been alternately a freshwater lake, an increasingly saline endorheic lake, and a dry desert basin, depending on river flows and the balance between inflow and evaporative loss.

A lake exists only during times it is replenished by the rivers and rainfall, a cycle that has repeated itself many times over hundreds of thousands of years,[9] perhaps cycling every 4. Evidence that the basin was occupied periodically by multiple lakes includes wave- cut shorelines at various elevations preserved on the hillsides of the east and west margins of the present lake, the Salton Sea. These indicate that the basin was occupied intermittently as recently as a few hundred years ago. The last of the Pleistocene lakes to occupy the basin was Lake Cahuilla, also periodically identified on older maps as Lake Le.

Conte or the Blake Sea, after American professor and geologist William Phipps Blake. Throughout the Spanish period of California's history, the area was referred to as the "Colorado Desert" after the Colorado River. In a railroad survey completed in 1. Valley of the Ancient Lake".

On several old maps from the Library of Congress, it has been found labeled "Cahuilla Valley" (after the local Native American tribe) and "Cabazon Valley" (after a local Native American chief – Chief Cabazon). Salt Creek" first appeared on a map in 1. Salton Station" is on a railroad map from 1. Until the advent of the modern sea, the Salton Sink was the site of a major salt- mining operation.[1. History during the 1. Original caption: Dry Bed of Colorado River Below Imperial Intake [..] River Diverted Into Imperial Canal. In 1. 90. 0, the California Development Company began construction of irrigation canals to divert water from the Colorado River into the Salton Sink, a dry lake bed.

After construction of these irrigation canals, the Salton Sink became fertile for a time, allowing farmers to plant crops.[1. Within two years, the Imperial Canal became filled with silt from the Colorado River.

Engineers tried to alleviate the blockages to no avail. In 1. 90. 5, heavy rainfall and snowmelt caused the Colorado River to swell, overrunning a set of headgates for the Alamo Canal. The resulting flood poured down the canal, breached an Imperial Valley dike, and ran down two former dry arroyos: the New River in the west, and the Alamo River in the east, each about 6. Over about two years, these two newly created rivers sporadically carried the entire volume of the Colorado River into the Salton Sink.[1. The Southern Pacific Railroad tried to stop the flooding by dumping earth into the canal's headgates area, but the effort was not fast enough, and the river eroded deeper and deeper into the dry desert sand of the Imperial Valley. A large waterfall formed as a result and began cutting rapidly upstream along the path of the Alamo Canal that now was occupied by the Colorado. This waterfall was initially 1.

Originally, it was feared that the waterfall would recede upstream to the true main path of the Colorado, becoming up to 1. As the basin filled, the town of Salton, a Southern Pacific Railroad siding, and Torres- Martinez Native American land were submerged.

The sudden influx of water and the lack of any drainage from the basin resulted in the formation of the Salton Sea.[1. The U. S. Navy conducted a preliminary inspection of the Salton Sea in January 1. Salton Sea Test Base (SSTB, run by Sandia Labs) was initially commissioned as the Naval Auxiliary Air Station, Salton Sea, in October 1.

The SSTB, just to the south- east of Salton City, originally functioned as an operational and training base for seaplanes.