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The Ubehebe Craters are a volcanic field in the northern Death Valley of California, consisting of 14–16 craters in a 3-square-kilometre (1.2 sq mi) area. The largest of the craters is the 800 metres (2,600 ft) wide and 235 metres (771 ft) deep Ubehebe Crater .
Ubehebe Crater (/ j u b i ˈ h iː b i / yoo-bee-HEE-bee) is a large volcanic crater of the Ubehebe Craters volcanic field in the northern half of Death Valley, in Death Valley National Park, California, United States.
Little is known about the history of the oldest exposed rocks in the area due to extensive metamorphism.This somber, gray, almost featureless crystalline complex is composed of originally sedimentary and igneous rocks with large quantities of quartz and feldspar mixed in. [1] The original rocks were transformed to contorted schist and gneiss, making their original parentage almost unrecognizable.
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.
In 2008 Teakettle Junction in December 2011. Teakettle Junction is a road junction in Inyo County, California. [1] [2] It lies at an elevation of 4,150 feet (1,260 m) in Death Valley near the Racetrack Playa and Ubehebe Crater.
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The name Death Valley was given by a group of pioneers lost in the valley around the years 1849-1850 during the winter season. The group assumed that the valley would become their “grave” even ...
A tourist visiting Death Valley had to be hospitalized after his bare feet briefly touched the blazing hot sands, causing him third-degree burns.. The tourist, an unnamed 42-year-old man from ...
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