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Badwater Basin is an endorheic basin in Death Valley National Park, Death Valley, Inyo County, California, noted as the lowest point in North America and the United States, with a depth of 282 ft (86 m) below sea level. [1] [2] Mount Whitney, the highest point in the contiguous United States, is only 84.6 miles (136 km) to the northwest. [3]
The property was sold to the Death Valley Hotel Company in 1956, and finally to the National Park Service. [2] Little remains of the structures but ruins. The works originally included a boiler, a tank for dissolved borax, and open tanks for crystallization of the borax. A stone building stood nearby to house the workers.
After discovery of Borax deposits here by Aaron and Rosie Winters in 1881, business associates William Tell Coleman and Francis Marion Smith subsequently obtained claims to these deposits, opening the way for "large-scale" borax mining in Death Valley. [3] Coleman constructed Harmony Borax Works and production of borax started in late 1883. [4]
Death Valley may be America's hottest national park, but it's also very cool. ... Visitors relish the wildflowers near Death Valley's Badwater Basin during a rare superbloom on Feb. 24, 2016.
Through exploratory holes drilled by the Pacific Coast Borax Company, prior to Death Valley becoming a national monument in 1934, it was discovered that the salt and gravel beds of the Devil's Golf Course extend to a depth of more than 1,000 feet (300 m). Later studies suggest that in places the depth ranges up to 9,000 feet (2,700 m).
Vinaya Vijay, right, and Vijay Parthasarathy wade through water at Badwater Basin, Thursday, Feb. 22, 2024, in Death Valley National Park, Calif. The basin, normally a salt flat, has filled from ...
Satellite images from NASA show how the lake in the California park’s Badwater Basin formed and then endured for months amid above-average rainfall in the lowest and driest spot in North America ...
Zabriskie Point is a part of the Amargosa Range located east of Death Valley in Death Valley National Park in California, United States, noted for its erosional landscape. It is composed of sediments from Furnace Creek Lake, which dried up 5 million years ago—long before Death Valley came into existence.