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The
Great Salt Lake is both the largest body of water between
the Great Lakes and the Pacific Ocean and the largest
salt lake in the western hemisphere. The Great Salt Lake
is the major remnant of Lake Bonneville, a large freshwater
lake of the Pleistocene era (75,000-7,250 B.C.) that occupied
much of western Utah. The lake occupies one of the basins
of the Great Basin, and is located at the western margin
of the Wasatch Mountains of the Rocky Mountain Range.
The
lake receives water from numerous perennial and intermittent
streams originating in the surrounding mountains, the
most important of which are the Bear, Weber, and Jordan
rivers. No streams empty from the lake, and its high salinity
is caused by the accumulation of minerals with no removal
and the accompanying water evaporation. The lake occupies
a broad level valley that has been created as deposits
eroded from the surrounding mountains have filled the
valley with sediments thousands of feet deep. The level
nature of the valley is responsible for wide variations
in the surface area of the lake, as a rise of only a few
feet during wetter years can increase the surface area
dramatically. In 1962 the lake elevation was 4,192 feet
above sea level, giving it a surface area of 969 square
miles (620,400 acres). In the early 1980s the lake reached
an elevation of 4,212 feet above sea level, giving it
a surface area of 2,300 square mile (1,472,000 acres).
The
existence of a large body of water in an arid region,
especially a salt lake, attracted early attention. Native
American cultures used the freshwater marshes and streams
around the lake for hunting and fishing. The first European
reports of the lake seem to have been by Baron Lahontan,
who reported in 1703 that he had seen a region west of
the Mississippi which contained a large salt lake. The
next recorded information about the lake came from the
Dominguez-Escalante expedition. Reaching Utah Lake in
1776, they were informed by Indians that it was joined
to a much larger lake to the north whose waters were "harmful
or extremely salty wherefore . . . anybody getting a part
of his body wet instantly feels severe itching around
the wet part." The most important effect of the Dominguez-Escalante
report was its inclusion of a map showing a river connecting
the Great Salt Lake to the Pacific Ocean. This mythical
river was later sought by explorers and settlers as a
route to the Pacific.
Trappers
explored the region of the Great Salt Lake, beginning
with Robert Stewart, who was at Bear Lake in 1812 but
apparently did not visit the salt lake. Later trappers
visited the lake, but is unclear who was first. Jim Bridger
reportedly saw the lake in 1824. In 1826 a group of four
trappers from the Rocky Mountain Fur Company spent twenty-four
days circumnavigating the lake, seemingly putting to rest
the idea of a river flowing from it to the Pacific Ocean.
In spite of this, the Frémont expedition of 1843-44
visited the Great Salt Lake in 1843 and searched for a
river flowing west to the Pacific, finally concluding
that the lake indeed occupied part of a great basin which
had no drainage to the sea.
Reports
of the valley of the Great Salt Lake reaching Mormon leaders
in Nauvoo, Illinois, prompted them to select it as a destination
by 1845, and the first Mormon pioneer party reached the
Great Salt Lake Valley on 22-24 July 1847. On 27 July
Brigham Young and other leaders of the group visited the
lake, and by August the lake was supplying salt to the
settlers.
The
high salt content of the lake has restricted its use,
but several resorts have existed on its shores from time
to time, the most famous being Saltair. From 1893 until
it burned in 1925, and again after its reconstruction
until drought isolated it in the 1930s, it was a major
recreation facility. More recently sailing has been a
popular activity at the lake. The lake has also been associated
with mining its salt and collecting its brine shrimp for
fish food. From the earliest Indians who obtained common
salt to modern industries extracting a variety of minerals
from its waters, from the tourists visiting the lake to
experience the buoyancy provided by its waters to locals
sailing its waters, the Great Salt Lake has remained a
valuable and unique part of America's geography.
See:
"Great Salt Lake," Utah Historical Quarterly
56 (1989); Dale L. Morgan, The Great Salt Lake (1947);
John C. Frémont, Report of the Exploring Expedition
to the Rocky Mountains in the Year 1842 and to Oregon
and Northern California in the Years 1843-44 (1845); Howard
Stansbury, An Expedition to the Valley of the Great Salt
Lake of Utah (1855).
Richard
H. Jackson
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