Ubehebe Crater (pronounced YOO-bee-HEE-bee) is located at the north tip of the Cottonwood Mountains. The crater is half a mile (one kilometer) wide and 500 to 777 feet (150 to 237 m) deep. The age of the crater is estimated from 2,000 to 7,000 years old.
The crater was formed when magma migrated close to the surface and the heat of the magma caused groundwater to flash into steam, throwing large quantities of pulverized old rock and new magma across the stony alluvial fan draped across the valley floor. The magma rose through a fault that lies along the western base of Tin Mountain. Movement on this fault was responsible for uplift of the entire Cottonwood Mountains range.
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). Earlier eruptions created a group of much shallower maars to the south and another to the west. Little Hebe is a spatter cone that grew in the middle of one of the largest maars in the south group. The only significant deposit of lava in the volcanic field is contained in Little Hebe.
All of the maar-forming eruptions sent out fallout debris that mantled a broad area around the volcanic field (dozens of steam explosions issued from Ubehebe alone). The resulting light to dark gray cinder deposits consist of finely fragmented volcanic rock mixed with pulverized bedrock and are thickest immediately next to Ubehebe (80 feet; 25 m). Rills and gullies that were 15 to 20 foot (4.5 to 6 m) deep dissected the area prior to the eruptions and were buried by the fallout. Erosion has since re-excavated these features, exposing layers of cinder that still overlay adjacent ridges.
A type of pyroclastic flow called a base surge was sent out of Ubehebe by one of the explosions. It started after a large column of debris was thrown skyward then began to collapse. A doughnut-shaped cloud of hot ash and gas (the base surge) sped 100 to 200 mph (160 to 320 km/h) from the base of the column while staying close to the ground, plastering the Ubehebe-facing side of all objects in the area.
Miocene-aged mostly reddish orange-colored conglomerate makes up the exposed bedrock in Ubehebe's walls. These sediments were deposited by streams and contain limestone, mudstone, quartzite and volcanic cobbles that are up to 8 inches (20 cm) in diameter. There is also a difference in color between these seabed sediments: On the left these sediments are yellowish in hue while on the right they are orange. The reason is due to a fault that separates the two different sedimentary units; over time at least 400 feet (120 m) of vertical displacement along this fault has resulted in the abutment of these two different sedimentary units. Fallout debris dip 30 feet (9 m) over the fault scarp on the pre-eruption surface but have not been offset by it.
There are three major trails at the crater. One trail goes from the parking area to the bottom of Ubehebe, a second circumnavigates the crater rim, while a third trail leads off to Little Hebe.
Winds at the rim of Ubehebe are very strong and often gust above 50 mph (80 km/h).
- Native American artifacts in the area indicate that 6,000 years is the most likely age although estimates of 2,000 years are common.
- Death Valley's Big Bang: Volcano "Potentially Active", National Geographic, January 25, 2012
- Ubehebe Crater: Possibly Younger but No Imminent Danger of an Eruption, Wired, January 24, 2012
- In Death Valley, ancient volcano gives scientists a surprise, Christian Science Monitor, January 24, 2012
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