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Ancient Lake Bonneville
Although he never visited the salt flats, the area
is named in honor of Captain B. L. E. Bonneville, whose expeditions in the
1830s proved the area was a part of the ancient basin.
During the last Ice Age, about 15,000 years ago,
Lake Bonneville was the size of Lake Michigan. It covered one-third of
present day Utah and parts of neighboring states. You can see traces of
the shorelines, representing different levels of the receding lake, etched
into the mountains surrounding the salt flats.
The Bonneville Salt Flats and the Great Salt Lake
are remnants of ancient Lake Bonneville. Wind and water combine to create
the flat surface of salt. Each winter, a shallow layer of standing water
floods the surface of the salt flats. During spring and summer, the water
slowly evaporates while winds smooth the surface into a vast, nearly
perfect, flat plain.
The salt surface contains potassium, magnesium
lithium, and sodium chloride (common table salt).
A Barrier of Salt
Humans have lived in the Great Basin for thousands
of years. Excavations at nearby Danger Cave have proven occupation of the
area as early as 10,300 years ago. While Native Americans adapted to the
desert environment, more recent arrivals found the area less hospitable.
By 1824, Jim Bridger and other mountain men explored
the Great Salt Lake desert region. The first recorded crossing of the
desert was made in 1845 by Captain John C. Fremont's survey party with
scouts Kit Carson and Joe Walker. Early the next year, 23 year old
Lansford Hastings retraced Fremont's train across the salt plain. Joe
Walker's writings warned emigrants not to attempt the untried route,
however, Hastings convinced several emigrant parties to follow him.
Despite Walker's warnings, the Donner-Reed party,
seeking a shortcut to California in 1846, attempted the "Hastings'
Cutoff." They failed to take enough water and lost a critical number
of oxen. Four of their wagons were abandoned just 10 miles northeast of
the salt flats. Time was lost, and the delay resulted in their late
arrival to the Sierra Nevada Mountains and their tragic winter.
Late, in 1910, the first permanent crossing of the
Bonneville Salt Flats was completed when the southern Pacific Railroad was
built linking Salt Lake City and San Francisco.
Typically, speed trials are scheduled throughout the
summer and fall. The events are open to the public. For more information,
contact the Bureau of Land Management, Salt Lake Field Office at (801)
977-4300.
Visiting the Salt Flats
The Bonneville Salt Flats is administered by the
Bureau of Land Management for public use and enjoyment. Due to its unique
geology, history, and scenic beauty, the Bonneville Salt Flats was
designated an Area of Critical Environmental Concern in 1985.
Help Preserve the Bonneville Salt Flats
Stay on existing roads or areas designated for
vehicles. Despite the appearance of a hard surface, much of the area is a
thin salt crust over soft mud. It easily breaks under the weight of a
vehicle.
Stay off the salt surface when it is covered by
water. When wet, the salt surface is soft and easily damaged by vehicles.
Furthermore, the salt water is highly corrosive and can short-out the
electrical system in your vehicle.
Be prepared for desert conditions. Temperatures can
exceed 100 degrees in the summer and drop well below 0 in the winter.
There are no facilities nor services on the salt
flats. Temporary facilities are available during racing events.
Overnight stays are prohibited on the salt flats.
Camping is encouraged on surrounding public lands. Private
campgrounds and hookups are available in nearby Wendover, ten miles west
of the Bonneville Salt Flats. Other accommodations and services are also
available in Wendover.
For Additional Information
Contact:
Bureau of Land Management
Salt Lake Field Office
2370 South 2300 West
Salt Lake City, Utah 84119
(801) 977-4300
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