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The crater is half a mile (one kilometer) wide and 500 to 777 feet (152 to 237 m) deep. The age of the crater is estimated from 2,000 to 7,000 years old. [1] In 2012, new evidence suggested that the crater may be as young as 800 years old, although this estimation was a lower bound, and it is still possible the crater is much older than that.
Death Valley National Park. 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. Many of the craters, though, are partially buried and ...
Ubehebe Peak. / 36.6910; -117.5856. Ubehebe Peak is a double summit mountain located within Death Valley National Park, in Inyo County, California. Ubehebe Peak rises over the west side of the Racetrack Playa, and lies at the south end of the Last Chance Range.
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. Later researchers discovered that the region had experienced substantial ...
Death Valley National Park averages about 2 inches of rain per year, the NPS said in the release. ... There are scatterings of wildflowers in Panamint Valley and Ubehebe Crater, the NPS reports ...
Death Valley. Death Valley is a desert valley in Eastern California, in the northern Mojave Desert, bordering the Great Basin Desert. It is thought to be the hottest place on Earth during summer. [3] Death Valley's Badwater Basin is the point of lowest elevation in North America, at 282 feet (86 m) below sea level. [1]
The hottest temperature recorded at Death Valley was 134 F (56.6 C) in July 1913, according to the National Park Service. Other parks have long-standing warnings for hikers.
The oldest rocks in the area that now includes Death Valley National Park are extensively metamorphosed by intense heat and pressure and are at least 1700 million years old. These rocks were intruded by a mass of granite 1400 Ma (million years ago) and later uplifted and exposed to nearly 500 million years of erosion.