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Death Valley National Park is a national park of the United States that straddles the California–Nevada border, east of the Sierra Nevada. The park boundaries include Death Valley , the northern section of Panamint Valley , the southern section of Eureka Valley and most of Saline Valley .
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 first movement of Ferde Grofé's Death Valley Suite is a symphonic musical portrayal of pioneer settlers trudging through the dry craggy peaks of the Funeral Mountains. Death Valley The winding road from Dante's View descends into the Funeral Mountains, Death Valley National Park.
The largest national park is Wrangell–St. Elias in Alaska: at over 8 million acres (32,375 km 2), it is larger than each of the nine smallest states. The next three largest parks are also in Alaska. The smallest park is Gateway Arch National Park, Missouri, at 192.83 acres (0.7804 km 2).
The Devil's Golf Course is a large salt pan on the floor of Death Valley. It was named after a line in the 1934 National Park Service guide book to Death Valley National Monument, which stated that "Only the devil could play golf" on its surface, due to a rough texture from the large halite salt crystal formations. [5]
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.
Death Valley is a desert valley in Eastern California, in the northern Mojave Desert, bordering the Great Basin Desert. It is thought to be the hottest place on Earth during summer. [3] Death Valley's Badwater Basin is the point of lowest elevation in North America, at 282 feet (86 m) below sea level. [1]
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.