Utah Water Science Center

Great Salt Lake

Filter Total Items: 5
Date published: July 6, 2020
Status: Active

Quantifying Nutrient Mass and Internal Cycling in Great Salt Lake

The Great Salt Lake (GSL) is an indispensable economic and ecological resource.  It provides critical habitat and food for millions of migratory birds, and generates nearly $200 million per year from recreational activities and the brine shrimp harvest industry (Bioeconomics, 2012).  These uses, habitat and aquaculture, rely on a balanced supply of nutrients in the Great Salt Lake to support...

Date published: January 23, 2018
Status: Active

Great Salt Lake Elevations

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.

Get current and historical lake levels here....

Contacts: Mike Freeman
Date published: January 16, 2018
Status: Completed

Earthshots 1972-2016: Satellite Images of Environmental Change

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...

Contacts: Robert Baskin
Date published: May 1, 2017
Status: Active

Great Salt Lake

Great Salt Lake is located on a shallow playa. Consequently, small changes in the water-surface elevation result in large changes in the surface area of the lake. This is particularly evident when the lake spills into the west desert at an elevation of about 4,215 feet, greatly increasing its area. The satellite imagery shows changes in the area of the lake from 1972, through the high-runoff...

Contacts: Cory Angeroth
Date published: March 21, 2017
Status: Active

Deep Brine Layer

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...