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Attraction · Salt Lake City, Utah

Great Salt Lake

The largest saltwater lake in the Western Hemisphere, the Great Salt Lake is a remnant of the prehistoric Lake Bonneville and is several times saltier than the ocean. Its shifting water levels expose or submerge landmarks like the Spiral Jetty, and its shoreline is a major stopover for millions of migratory birds each year.

Visitor guide

About Great Salt Lake

The Great Salt Lake is a shallow, hypersaline lake in northern Utah and the largest saltwater lake in the Western Hemisphere, according to Britannica as cited by Wikipedia. It is the shrunken remnant of ancient Lake Bonneville and a terminal lake, meaning it has no outlet to the ocean and loses water only by evaporation.

Origins

Lake Bonneville, the Ice Age lake that preceded it, covered roughly 22,400 square miles at its peak, about ten times today's area, and its old shorelines are still visible as terraces along the mountainsides of the region. As Bonneville shrank, the Great Salt Lake remained in the lowest part of the basin. The USGS describes the lake as sitting at the bottom of a 35,000-square-mile drainage basin, fed mainly by the Bear, Weber and Jordan rivers, which together carry about 2.2 million tons of salt into the lake each year, according to the USGS.

Size and salinity

Because the lake is shallow, its area swings with small changes in level. The historical average area from 1847 to 1986 is given as about 1,700 square miles, the USGS records the historic high water level on June 3, 1986, when the lake covered approximately 2,300 square miles, and says it covered less than 1,000 square miles in 2022; other sources give different area figures. Salinity depends heavily on level and location. The USGS reported that south of the railroad causeway it ranged from 6 to 27 percent over 22 years, which is roughly 2 to 7 times saltier than the ocean. A railroad causeway built in the 1950s divides the lake into a southern arm and a saltier northern arm, and a bridge opened in 2016 allows some exchange of water between them. The northern arm, with its higher salinity, can turn pink.

Life on the lake

The lake is too salty for fish, but the USGS describes an ecosystem of more than 30 species, anchored by brine shrimp and brine flies. Brine shrimp cysts are harvested commercially and supply the aquaculture industry worldwide. Millions of migratory and nesting birds use the lake and its shoreline, feeding on the shrimp and flies; Wikipedia notes the lake hosts what is described as the largest staging population of Wilson's phalaropes in the world. Mineral extraction, including salt, also removes about 2 million tons from the lake each year according to the USGS.

The lake today

Drought, a changing climate and upstream water use have shrunk the lake in recent decades, and Utah agencies and researchers continue to track and debate its future; the USGS reports that the southern arm reached a record low water surface elevation of 4,188.5 feet on November 7, 2022, in a record that dates back to 1847. For current lake levels and conditions, check the Utah Geological Survey, the USGS or Utah State Parks.

Seeing it

The lake can be experienced from several vantage points. Antelope Island State Park, reached by causeway, offers beaches and trails, and Wikipedia notes the lake also contains other islands, though counts differ by source. Shoreline conditions vary with water level, so check the state for current access.

With a private tour

A private vehicle with a driver and door-to-door pickup can combine the lake with other Salt Lake City stops, so your group is not tied to a fixed schedule.

Frequently Asked Questions About Great Salt Lake

It is a terminal lake with no outlet, so dissolved minerals carried in by rivers stay behind as water evaporates.
The USGS reported salinity south of the causeway ranging from 6 to 27 percent over 22 years, roughly 2 to 7 times saltier than the ocean.
Lake Bonneville was an Ice Age lake covering about 22,400 square miles at its peak, and the Great Salt Lake is its shrunken remnant.
The lake is too salty for fish but supports brine shrimp, brine flies and millions of migratory birds.
The Bear, Weber and Jordan rivers are its three main sources, carrying dissolved minerals into the lake.
The lake is shallow, so small changes in water level change its surface area noticeably.
Its historical average area is about 1,700 square miles, though the USGS says it covered about 2,300 square miles at its 1986 high and less than 1,000 square miles in 2022.
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