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The last active mine in Death Valley closed in 2005. [1] The location was discovered by a miner named Jack Keane. Keane and a partner named Domingo Etcharren had scouted the area, called Chloride Cliffs, and had located a potential silver mine. Etcharren eventually left while Keane stayed behind to scout the area more thoroughly.
Gower Gulch is named after Harry P. Gower, an official of the Pacific Coast Borax Company and co-owner of the Furnace Creek Inn and Ranch, before Death Valley became a national monument. The gulch contained mines, camps, and roads during the late 19th century and early 20th century.
Xanterra Parks & Resorts owns and operates a private resort, the Oasis at Death Valley, [39] which comprises two separate and distinct hotels: the Inn at Death Valley is a four-star historic hotel, and the Ranch at Death Valley is a three-star ranch-style property reminiscent of the mining and prospecting days.
It sprang up near the most promising discovery, the Montgomery Shoshone Mine, which in February 1905 produced ores assayed as high as $16,000 a ton, [30] equivalent to $543,000 a ton in 2023. [27] Starting as a two-man camp in January 1905, Rhyolite became a town of 1,200 people in two weeks and reached a population of 2,500 by June 1905.
NO. 441 BURNED WAGONS POINT - Near this monument, the Jayhawker group of Death Valley '49ers, gold seekers from the Middle West who entered Death Valley in 1849 seeking a short route to the mines of central California, burned their wagons, dried the meat of some oxen and, with surviving animals, struggled westward on foot. [11]
Panamint City (est. 1873) was a mining town in the district, formerly in the central section of the range. [7] The historic mining community of Ballarat (est. 1890s), also in the district, is now a ghost town. [7] The Gold Hill Mining District (est. 1875) was in the southwestern section of the range, at the northeast end of Butte Valley. [8]
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Manly Beacon and Red Cathedral viewed from Zabriskie Point. The Amargosa Chaos is a series of geological formations located in the Black Mountains in southern Death Valley.In the 1930s, geologist Levi F. Noble studied the faulting and folding in the area, dubbing it the "Amargosa chaos" due to the extreme warping of the rock.