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Ubehebe Crater in Springtime. Geologists call the resulting large steam explosions hydrovolcanic or phreatic eruption and the pits created are known as maars.Ubehebe was the last and largest in a series of similar eruptions in the immediate area (its eruption exceeded the tensile strength of the bedrock by 10 times).
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 Crater is the largest of more than a dozen of in the Ubehebe Craters field. As groundwater exploded into steam due to the heat of magma underneath, an empty pit was left behind and the debris spread around the field. Erosion over the millennia since the eruption revealed multi-colored stripes on the crater walls dating to the Miocene ...
The eye-opening 600-foot (183-meter) Ubehebe Crater dates back over 2,000 years. And Zabriskie Point is a prime sunrise viewing spot. Eugen Chen from Taiwan called the park “beautiful” and an ...
One example of such a feature is the roughly 2000-year-old and 800 feet (240 m) deep Ubehebe Crater in the northern part of the park; [28] nearby smaller craters may be less than 200 to 300 years old. [29] Sediment filled the subsiding Furnace Creek Basin as the area was pulled apart by Basin and Range extension.
The highest point surrounding the Racetrack is the 5,678-foot (1,731 m) high Ubehebe Peak, rising 1,964 feet (599 m) above the lakebed 0.85 miles (1.37 km) to the west. [ citation needed ] The playa is in the small Racetrack Valley endorheic basin between the Cottonwood Mountains on the east and Nelson Range to the west.
Mount Bachelor, formerly named Bachelor Butte, is a dormant stratovolcano atop a shield volcano in the Cascade Volcanic Arc and the Cascade Range of central Oregon.Named Mount Bachelor because it stands apart from the nearby Three Sisters, [4] it lies in the eastern segment of the central portion of the High Cascades, the eastern segment of the Cascade Range.
Ubehebe Crater is another distinctive geologic feature and visual landmark in this northern section of the park. Saline Valley is located to the west, and the Eureka Valley Sand Dunes to the north. The south end of Eureka Valley Road is nearby, located 2.5 miles east of Ubehebe Crater, so visitors planning to tour both The Racetrack and Eureka ...