Facts About Utah's Great Salt Lake

Geography
A combination of size and salt content makes Utah's Great Salt Lake unique among lakes in the western
hemisphere. The current surface elevation of the Great Salt Lake is 4,203 feet. It is 75 miles long and 30
miles wide with a surface area of 1,500 square miles. To emphasize its size, the Great Salt Lake is the
largest lake west of the Mississippi River, larger than the states of Rhode Island and Delaware.
The greatest depth in the lake is 40 feet with the average depth being
14 feet. The historic low level of the lake has been 4,193 feet which
occurred in 1963 and the historic high elevation is 4,212 recorded in
1987.
Antelope Island is the largest of the lake's ten islands. Other islands
include Fremont, Stansbury, Carrington, Cub, Gunnison, Dolphin,
Badger, Egg and Bird Island.
Major water sources for the Great Salt Lake include the Bear River at
1,200,000 acre feet per year; precipitation at 1,000,000 acre feet per
year; the Jordan and Weber Rivers at 400,000 acre feet per year each.
North & South
The great body of briny water was an obstacle in the path
of completing the transcontinental railroad line. The tracks
were routed over the Promontory Mountains where on May 10,
1869, a golden spike was driven to mark completion of the
first transcontinental railroad. This route was not easy
because of the steep mountains. In 1903, a twelve-mile bridge
was built across the Great Salt Lake. In 1959, a solid-fill
causeway was built to replace the old trestle. This causeway
still separates the north (Gunnison Bay) and south (Gilbert
Bay) ends of the lake. This separation has caused the north
end of the lake to have a higher mineral and salt
concentration as well as higher purity as the industrial
activity takes place on the southern region of the lake.
According to a geological survey issued by the U.S.
Department of the Interior, the salinity of Gilbert Bay
declined from nearly 15 percent in late 1995 to 11 percent in
late 1997. The salinity in Gunnison Bay fluctuated only 1 to 2
percent (the average is 28 percent) during the same time.
FAQs about the Great Salt Lake
How much salt is in the lake?
The total amount of salt dissolved in the Great Salt Lake
is about 4.5 to 4.9 billion tons. As the lake rises, its
salinity drops because the same amount of salt is dissolved in
more water. The lower the lake level, the saltier it becomes.
In the past, the lake's salinity has ranged from a little less
than 5 percent (which is just above sea water) to nearly 28
percent (beyond which water cannot hold more salt).
Can I float in the Great Salt Lake?
You can easily float in the lake if the water is salty
enough. At the lake's average elevation of 4,200 feet, it is
less salty and, therefore, less buoyant. Swimmers float easily
in the north arm because it is twice as salty as the south arm.
Why is the lake so salty?
As water flows over or moves beneath the Earth's surface,
it dissolves minerals from the soils and rocks. The streams
that originate in the Wasatch Range and other nearby mountains
all flow into the Great Salt Lake, bringing in water with
varying percentages of dissolved minerals. Since the lake has
not outlet, all of these minerals remain in the lake.
Science
Biology
Due to the high
salinity of the water, most forms of aquatic life cannot live
in the lake. Certain species have adapted and, in fact, have
flourished. Algae and protozoa exist in the
lake and because of their simplicity in make up, they thrive
in the otherwise harsh environment. The more advanced life
forms are the called brine fly and brine shrimp. Both exist in
large numbers.

Gulls, pelicans, cormorants, terns, and heronsmake Great Salt
Lake their home during the nesting season. The gulls and
pelicans are by far the most numerous.
Weather
Locals call it the
"lake effect." More than 24 inches of snow have been known to
fall in a 24 hour period along the Wasatch Mountains when a
naturally intense storm passes over the area. The warmer air
from the lake rises, colliding with the colder, stormy air,
thereby resulting in the heavy amount of snowfall particular
to the Wasatch front area. These "lake effect" storms usually
occur in the spring or fall and can bring intense
thunderstorms as well as the heavy snowfall.
History
The origin of the
Great Salt Lake can be traced back to ancient Lake Bonneville
which covered most of Western Utah and small parts of Idaho
and Nevada during the Ice Age (between 23,000 and 12,000 years
old). In the warmer, dry period after the ice age, Lake
Bonneville receded and the Great Salt Lake is the remnant of
that ancient lake.
Recent History
Reports and rumors of the
existence of a huge salty lake somewhere in the west were
heard of for more than a hundred years before any white man
actually visited its shores.
The first authentic
information about the lake came from the Dominguez-Escalante
expedition of 1776. Leaders of the group learned from area
natives of the lake which was extremely salty. The group named
it "Lake Timpanogos" but did not actually travel to see the
lake.
While James Bridger is the
first white man known to have seen the lake, John C. Fremont
was the first to scientifically examine the lake in 1843.
Fremont and his crew were the first to accurately map the area
and one of the ten islands bears his name.
According to the Deseret
News, one of Utah's daily newspapers, Shoshone and Goshute
Indians used to live on or near Antelope Island. A son of
Chief Wanship and his family were living on Antelope Island
when Fremont explored the lake.
For more information about
Utah's Great Salt Lake, please click the following links.
Friends of Great Salt Lake
Mineral Resources International is proud to be a corporate sponsor of Friends of Great Salt Lake.
Founded in 1994, its mission is to preserve and protect the
Great Salt Lake ecosystem and increase public awareness and
appreciation of the lake through education, research, and
advocacy.
United States Geological Survey
The Great Salt Lake (Deseret News)
Great Salt Lake Map (Utah Automated Geographic Reference
Center)
Great Salt Lake Satellite Map (USGS)