bonneville salt flats water

In those days, it was common for fur trappers to name significant landmarks after their employers, perhaps in an effort to gain favor or better wages. The potential for racing at Bonneville was first recognized in 1896 by W.D. According to Intrepid Potash, which has mineral rights to the waterway, the water is more a brine mixture and comes from a series of ditches in the nearby Salt Flats. However, still very much worth the detour! The flats are about 12 miles long and five miles wide, covering about 46 square miles in total. You can imagine how big this ancient lake must have been because The Great Salt Lake is a mere remnant of it. In addition, the Utah Highway Patrol has indicated that parking along I-80 to access to the canals is illegal and extremely dangerous due to the proximity to the interstate highway.No overnight camping on the salt flats.

The Bonneville Salt Flats are a densely packed salt pan in Tooele County in northwestern Utah. Rishel returned and convinced daredevil Teddy Tezlaff to attempt an automobile speed record on the flats. The Bonneville Salt Flats are comprised of approximately 90% common table salt.Access to the area is via a paved road. Several SUVs actually drove into the water and seemed to be having a blast. In the following year, Fremont's route across the flats would come to be known as the Hastings Cutoff route along the California Trail.© Utah Office of Tourism. The property is public land managed by the Bureau of Land Management and is known for land speed records at the "Bonneville Speedway". In 1845, John C. Fremont and his U.S. government-sponsored exploratory expedition crossed through the very heart of the Salt flats in an effort to find a shorter overland route to the Pacific. The Bonneville Salt Flats are a 30,000 acre expanse of hard, white salt crust on the western edge of the Great Salt Lake basin in Utah.

After 2 hours of driving to get here we cracked up laughing as we sped down the 'runway' toward the salt flats only to screech to a halt at the water's edge.

Parts of Utah’s Bonneville Salt Flats are carved into canals and ponds used by Intrepid Potash to extract valuable minerals from the rich brines coursing through them.

When the brine has reached an optimum concentration in early spring, it is pumped to the north side of Interstate 80 via canals and discharged onto the southern section of the Bonneville Salt Flats near the access road.

These minerals include gypsum (commercially used to make household wallboard) and halite (common table salt). Its vast!

"Bonneville" is also on the National Register of Historic Landmarks because of its contribution to land speed racing. The lake ceased to exist about 14,000 years ago when most of its water released in a single natural cataclysm called the Bonneville Flood. The paved road just stops with no warning then it is water and salty mud.Just off Hwy 80, the flats were completely flooded about 3 miles off the hwy exit. Really interesting to see it covered in a thin layer of water.

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