Causeway

Great Salt Lake Elevations The United States Geological Survey (USGS) has been collecting water-surface-elevation data from Great Salt Lake since 1875 and continuously since October 1902. The north part of the lake has been monitored since April 1966. On October 18, 2021, the southern portion of the Great Salt Lake set a new record low average daily elevation of 4,190.2 feet, which is about 1.2...

In July 2021, the southern portion of the Great Salt Lake reached a new historic low, with average daily water levels dropping about an inch below the previous record set in 1963, according to U.S. Geological Survey information collected at the SaltAir gage. -Find all news releases associated with the Great Salt Lake from the News Tab at the top of this page.

Dramatic changes in lake levels are observed in these images from 1972-2016. The completion of the Railroad Causeway in 1959 divided the Great Salt Lake in half. Because all of the freshwater inflows enter the southern part of the lake and evaporation is greater in the northern part, the north arm became much more saline than the south; well defined in the satellite images. Several years of...

In 1959, a solid-fill railroad causeway was constructed across the middle of the Great Salt Lake. The construction of the causeway divided the lake into two parts; the north (Gunnison Bay) and the south (Gilbert Bay). By 2013, water flowed from one side to the other through only two culverts near the center of the causeway. In December 2013, concern about the structural integrity of the culverts...