Agricultural drain in the Imperial valley, California, the source of the Salton Sea.


Victor M. Ponce

The Salton Sea is the largest lake in California, encompassing 378 square miles in Imperial and Riverside counties, in the Southeastern edge of the state.

Strictly speaking, it is not a sea but a geological depression tucked between mountain ranges and lying below sea level.

In the past century, it has been used as the repository for agricultural wastewaters originating in the Imperial valley, which neighbors the Salton Sea to the South.

The sea is slowly deteriorating for its other uses, and the question has been raised: What to do about this?

Should the sea, effectively a sink for wastewaters, be left to degrade slowly with time?

Or, should it be restored to an optimal or target salinity level?

This document explores the various issues surrounding the controversy.


The geologic depression where the Salton Sea is located was caused over geologic time by mountain uplift and associated subsidence. > As the mountains in the vicinity grew, subsidence of the Earth's mantle led to the depression, with its lowest point at -278 ft below mean sea level. > The neighboring Colorado river, in its quest to reach the ocean, eroded and transported billions of tons of sediment (boulders, sand, silt and clay) towards its mouth at the Gulf of California.

Over geologic time, it formed, near its estuary, the natural levees which isolated the Salton depression, protecting it from the eventual incursion of the ocean to the South.

Any water reaching the depression, either from local runoff or from the Colorado river during major floods, eventually evaporated, leaving a dry lake bed most of the time.

Runoff in the depression was endorheic, meaning that the lowest point, to which runoff tends naturally, is not at the basin's perimeter, but rather somewhere in the middle.

Thus, the Salton depression and its status prior to human intervention was closely linked to the prevailing geology and geomorphology, and to its peculiar geographical location, near the mouth of a great river, the Colorado, which historically has carried a lot of sediment.


In 1905, a diversion was engineered in the Colorado river, in Baja California, Mexico, a few miles South of Yuma, Arizona, for the purpose of conveying water to irrigate lands in the Imperial valley, in Imperial County, California, located to the Northwest.

An unexpected flood caused the diversion to fail, and the Colorado river changed course, first flowing West and then North in the direction of the Salton depression.

By the time the river was brought under control, two years later, in 1907, the water had filled the depression to the level of -195 ft, effectively creating the Salton Sea.

Left on its own, the water in the sea would have eventually evaporated.

This is because the region's mean annual precipitation is only about 2.3 inches, while the mean annual evaporation is 70 inches.

By the early 1920's, the sea had reached a low of -250 ft.

However, in 1928, Congress acted to designate the lands within the Salton basin below -220 ft as storage for wastes and seepage water from irrigated lands in Imperial valley.

Since then, the sea has been used mainly as a repository for agricultural wastewaters, with the water level rising gradually to its present -236 ft. (2023)

The average depth of the sea is about 26 ft, and the maximum is 42 ft (2023).


In 1907, at the time of the sea's origination, the average salinity of the water was about 3,500 parts per million.

With the agricultural wastewaters came a diversity of solids, mostly salt ions, which contributed to the lake's increase in salinity.

Up to the year 2005, the lake was close to hydrologic equilibrium, with inflows closely matching outflows through evaporation.

Since that time, due to decreased inflows, the lake has been decreasing in area and elevation. The current elevation (2023) is -236 ft.

The solid ions, however, among them, notably, sodium (Na+) and chloride (Cl-), are being left behind to accumulate in the lake profile.

The high solubility of sodium chloride assures that, left on its own, the sea's salinity will continue to increase with time.

Levels of salinity have presently (2023) reached about 60,000 parts per million, making the sea about 70% saltier than the ocean.

The origin of the salts and other mineral constituents entering the Salton Sea can be traced to four sources:

  1. The salt already present in the soil profile (local or old geologic salt),

  2. The salt brought in with the irrigation water (imported or new geologic salt),

  3. The salt produced by the weathering of the soil minerals as a result of irrigation (local or old anthropogenic salt), and

  4. The salt leached from the soil profile because of excessive fertilization (imported or new anthropogenic salt).


Initially, the Salton Sea supported a community of freshwater fishes that came with the Colorado river water.

As salinity increased through the years, the original freshwater fish disappeared.

Between 1929 and 1956, the California Department of Fish and Game made numerous transplants of both fish and invertebrates with the aim of developing a sport fishery in the sea.

Of the numerous sport-fishery species intentionally transplanted, only three, corvina, sargo, and bairdella, survived.

Laboratory research has shown that spawning of corvina does not take place at salinity levels exceeding 45,000 parts per million.

Other recreation activities at the sea initially included boating, water skiing, hiking, and bird watching. As the lake has deteriorated in its water quality, so do its other uses.


The impact of increased salinity is not limited to fisheries resources.

It is also likely to affect wildlife resources, since the Salton Sea is in the Pacific Flyway, which sustains numerous migratory bird species, particularly the waterbirds.

The latter represent the higher trophic levels of food chains in the Salton Sea and surrounding areas.

Nearly 400 bird species have been observed at the sea, about half of the 900 bird species known to exist in the North American continent.


As it currently stands, the Salton Sea serves three purposes:

  1. A convenient repository for agricultural wastewaters,

  2. A resource for fisheries and outdoor recreation, although this use has been diminishing since the 1979s, and

  3. A resource for wildlife.

Since the natural state of the sea is a dry lake bed, all three of these uses are artificial.

The first use is a logical consequence of extensive irrigation in the Imperial valley, which results in substantial economic benefit to the local growers and, by extension, to the State of California.

The second use admittedly would not exist if it were not for the first, and the existence of the third use is related to the second.

Thus, in the Salton Sea, the needs of the agricultural enterprise are closely intertwined with society's perceived needs for recreation and wildlife.

In 2003, a decision was made to effect an annual transfer of 200,000 acre-feet of water from the Imperial valley to San Diego County, for urban use.

After 2019, with the transfer in full force, the reduced inflows to the sea will produce a shift in the hydrologic equilibrium to a lower sea level. In the past 18 years, the lake elevation has decreased 9 ft, reducing its footprint accordingly.


Left on its own, the lake's salinity will continue to increase gradually, eventually impairing its other uses.

The fish will disappear, and this will affect the wildlife.

Only one use will remain: that of serving as a dump for the wastewaters of the agricultural enterprise.

The veritable brew of chemical constituents and elements, including selenium, will have to be monitored carefully to avoid a repetition of the Kesterton Reservoir incident in California's San Joaquin valley, in the 1980's.

In this case, a much smaller human-made lake, also a repository for agricultural wastewaters, was used by birds who eventually became sick and perished from ingesting large quantities of selenium and other toxics.

The latter, brought in trace amounts with the water, had accumulated to concentrations that became lethal to the unsuspecting birds.


Barring no action, the alternative is to restore the sea so that it can continue to serve its other purposes, i.e., recreation and wildlife.

In principle, this requires reducing the salinity of the Salton Sea to a level comparable to that of the ocean.

This undertaking is technologically complex, energy-intensive and costly, with the price tag likely to run into the billions of dollars.

Extracting sodium chloride out of water is at best a difficult proposition.

The situation is complicated by the fact that the salts of the Salton Sea are of many types.

Sodium and chloride constitute only about 60% of the salt ions, so evaporation will produce a mix of salt ions that will be difficult to commercialize.

Salt separation hinges upon the development of appropriate markets for the various salt products.

To this date, no restoration strategy is without its pitfalls.

Geographical location of the Salton Sea

Fig. 1   Geographical location of the Salton Sea.