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Death Valley, California, July 3, 2017, Sentinel-2 true-color satellite image, scale 1:250,000. Map showing the system of once-interconnected Pleistocene lakes in eastern California (USGS) Death Valley is a graben—a downdropped block of land between two mountain ranges. [13]
Death Valley is the fifth-largest American national park and the largest in the contiguous United States. It is also larger than the states of Rhode Island and Delaware combined, and nearly as large as Puerto Rico. [10] In 2013, Death Valley National Park was designated as a dark sky park by the International Dark-Sky Association. [11]
The World Wildlife Fund lists the Mojave Desert as relatively "stable/intact". [2] Various habitats and regions of the Mojave Desert have been protected by statute. Notably, Joshua Tree National Park, Death Valley National Park, and the Mojave National Preserve by the California Desert Protection Act of 1994. (Pub.L. 103–433). Various other ...
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 ...
Death Valley has a hellish summertime climate almost unlike any other spot on the planet: "With an average daily high of 115 degrees and a low of 87 during the month of July, Death Valley is far ...
Little is known about the history of the oldest exposed rocks in the area due to extensive metamorphism.This somber, gray, almost featureless crystalline complex is composed of originally sedimentary and igneous rocks with large quantities of quartz and feldspar mixed in. [1] The original rocks were transformed to contorted schist and gneiss, making their original parentage almost unrecognizable.
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.
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