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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.
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.
The side road to Aguereberry Point successively traverses the shaly Johnnie Formation, the white Stirling Quartzite, and dark quartzites of the Wood Canyon Formation; at the Point itself is the great light-colored band of Zabriskie Quartzite dipping away toward Death Valley. [9]
Many of Death Valley National Park's most well-known features, such as Zabriskie Point and Artists Drive are located in or are part of the Amargosa Range. The Amargosa mountains are also home to Corkscrew Peak, so named because it resembles a corkscrew.
Death Valley is known as America’s hottest, driest and lowest national park. It holds the Guiness World Record for the highest temperature ever recorded anywhere: 134 degrees on July 10, 1913.
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 ...
Telescope Peak (Timbisha: Chiombe) is the highest point within Death Valley National Park, in the U.S. state of California. It is also the highest point of the Panamint Range, and lies in Inyo County. From atop this desert mountain one can see for over one hundred miles in many directions, including west to Mount Whitney, and east to Charleston ...
A temporary lake formed in Death Valley National Park due to intense rain hitting California. Nature lovers took advantage of the rare event.
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