Great Salt Lake
The Great Salt Lake is a large body of salt water, N Utah. The lake is irregular in shape and is about 121 km (about 75 mi) long from N to S and 48 to 80 km (30 to 50 mi) wide. Its average depth is about 6 m (about 20 ft.), but great seasonal variations occur. The lake is deepest in the spring, when it is fed by the melting snow from the nearby Wasatch Mts. to the E. The size of the lake has diminished markedly since the 1860s, to an average area of 4403 sq. km (about 1700 sq. mi). Unusual drainage conditions increased the area in 1986 to 6343 sq. km (2450 sq. mi) and raised the altitude from 1280 m (about 4200 ft.) by 3.35 m (11.5 ft.).
Great Salt Lake occupies a portion of what was, in Pleistocene times, the bed of the great Bonneville Lake. The present lake has no outlets and loses water naturally only by evaporation, which concentrates the dissolved salts carried into the lake by its tributaries and causes its salinity. The lake is fed from Utah Lake to the S through the Jordan R., by the Weber R. to the E, and by Bear R. to the NE.
The salinity of Great Salt Lake, normally about 23 parts per 1000, decreased as the area increased. The chief constituent of the dissolved salts is sodium chloride, which is recovered in commercial quantities. The lake has been estimated to contain more than 5 million metric tons of sodium chloride in solution. A few species of marine life have been found, including a brine shrimp variety.
The lake was first noted on maps prepared in the 1770s by two Roman Catholic priests, Silvestre Vélez de Escalante (fl. 1769–79) and Francisco Atanasio Domínguez, who had never seen it. Several fur traders later visited (1824–25) the lake; it is believed that the American fur trapper James Bridger was the first to reach it. The lake was explored by the American soldier Benjamin de Bonneville in the 1830s and by (1843–45) the American general John Charles Frémont. In 1849 the first survey of the area was made by a party of U.S. Army engineers.
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