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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.
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]
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.
The Death Valley View Hotel operated full-time from 1927 until 1930, the year the Death Valley Railroad ceased to function. After 1930 the hotel was used as overflow accommodations for the Furnace Creek Ranch and Inn through the 1950s. [9] [3] The Death Valley Conservancy is the current caretaker of Ryan Camp. [10]
A map of the Death Valley Railroad running from Death Valley Junction all the way up to the mines at Ryan near Colemanite. The Death Valley Railroad (DVRR) was a 3 ft (914 mm) narrow-gauge railroad that operated in California's Death Valley to carry borax with the route running from Ryan, California, and the mines at Lila C, both located just east of Death Valley National Park, to Death Valley ...
The creation of the monument resulted in a temporary closing of the lands to prospecting and mining. However, Death Valley was quickly reopened to mining by Congressional action in June 1933. As improvements in mining technology allowed lower grades of ore to be processed, and new heavy equipment allowed greater amounts of rock to be moved ...
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.
Skidoo is representative of the boom towns that flourished in Death Valley during the early 20th century. The town's livelihood depended primarily on the output of the Skidoo Mine, a venture operating between 1906 and 1917. During those years the mine produced about 75,000 ounces of gold, worth at the time more than $1.5 million.