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The Quaternary tectonics of the Death Valley area show the increasing impact of right-lateral strike-slip faulting. Death Valley itself is currently an active pull-apart basin developed between the Northern and Southern Death Valley Faults, with mainly normal faulting along the Black Mountains Fault zone between these two major strike-slip ...
The north-northwest end of the Walker Lane is between Pyramid Lake in Nevada and California's Lassen Peak [1] [2] where the Honey Lake Fault Zone, the Warm Springs Valley Fault, and the Pyramid Lake Fault Zone [3] meet the transverse tectonic zone forming the southern boundary of the Modoc Plateau and Columbia Plateau provinces.
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.
The Death Valley Fault Zone (DVFZ) is a right lateral-moving (dextral) geologic fault in eastern California. It runs from a connection with the Furnace Creek Fault Zone in the Amargosa Valley southward to a junction with the Garlock Fault. It is considered an integral part of the Walker Lane.
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.
Here’s what we know about the valley dubbed as one of the hottest places on Earth. In 2022, over 1 million people visited the national park. Here’s what we know about the valley dubbed as one ...
But that range is lower than the actual temperature in Death Valley, California. A persistent and deadly heat wave is still baking parts of the country. Almost a third of the country, stretching ...
Fault-block mountains often result from rifting, an indicator of extensional tectonics. These can be small or form extensive rift valley systems, such as the East African Rift zone. Death Valley in California is a smaller example.