Context (LM): Scientists have discovered a massive lithium deposit beneath California’s Salton Sea, holding an estimated 18 million tons of lithium.
Salton Sea
The Salton Sea is a shallow, saline lake located in the California desert.
The Sea was created in 1905 when water from the Colorado River spilled out of a poorly constructed California Development Company irrigation system and into a basin in the desert.
The lake then expanded in size for several years until workers were able to put a stop to the flow.
The lake lies on the San Andreas Fault within the Salton Trough, which stretches to the Gulf of California in Mexico.
The lake is bordered on the south by the rich agricultural areas of the Imperial Valley, on the west, by Anza-Borrego Desert State Park, and on the north by the Coachella Valley.
It is an endorheic lake, meaning that its waters have no outlet to the ocean.
It has been maintained by irrigation runoff coming from the Imperial and Coachella valleys and nearby rivers ever since its formation.
It is currently 228 feet below sea level.
Its salinity (some 45 parts per thousand) far exceeds that of seawater.
The Sea is an important stopping point for migratory waterfowl and serves as a critical habitat for birds moving south to Mexico and Central America.
Lithium
Lithium is a non-ferrous, soft, silvery-white alkali metal. It is also called ‘white gold’ due to its high demand for rechargeable batteries.
Under standard conditions, it is the least dense metal and the least dense solid element.
Like all alkali metals, lithium is highly reactiveand flammable, so it must be stored in a vacuum, inert atmosphere, or inert liquid (such as purified kerosene or mineral oil).
It exhibits a metallic lustre. But it corrodes quickly in the air to a dull silvery grey, then black tarnish.
It never occurs freely in nature but occurs mainly as pegmatitic minerals.
Due to its solubility as an ion, it is present in ocean water and commonly obtained from brines (high-concentration salt solution in water).
Lithium metal is isolated electrolytically from a mixture of lithium chloride and potassium chloride.
Pegmatite is a coarse-textured igneous rock that forms during the final stage of magma’s crystallisation. It contains large crystals and minerals rarely found in other types of rocks.
Top producers of lithium: 1st Australia > 2nd Chile > 3rd China > 4th Argentina > 5th Zimbabwe