Owens Lake.
Owens Lake, which is the “sink” of Owens River, has an area of about 110 square miles. Its waters are heavily charged with salt and alkaline minerals. One United States standard gallon (8⅓ pounds, or 231 cubic inches) of the lake water contains 4,422.25 grains of solid matter, sodium carbonate and sodium chloride predominating and aggregating 2,561.83 grains.
The water of the lake contains only a trace of borax. It is evaporated on a large scale near Keeler, for the valuable alkaline minerals it holds in solution. The water of Owens Lake contains a much greater quantity of mineral matter than that of the Dead Sea. In Dead Sea water there is only 1,680 grains of solid matter to the United States gallon. Dead Sea water is evidently less salt than that of many of the lakes of the Great Basin region, as fish are found in it at and near the mouths of tributary streams, and in places along its shores shell-fish are to be seen.