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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]
Albireo / æ l ˈ b ɪr i oʊ / [23] is a binary star designated Beta Cygni (β Cygni, abbreviated Beta Cyg, β Cyg). The International Astronomical Union uses the name "Albireo" specifically for the brightest star in the system. [ 24 ]
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.
ˌ b ɛr. i / [1] is a promontory and tourist viewpoint in the Panamint Range, within Death Valley National Park in Inyo County, eastern California. The point's elevation reaches 6,433 ft and is named for Jean Pierre "Pete" Aguereberry, a Basque miner who was born in 1874, emigrated from France in 1890, and lived at and worked the nearby Eureka ...
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 eastern portion begins at US 395 southeast of Olancha, heads east through Death Valley National Park, and ends at State Route 127 at Death Valley Junction. The 43.0-mile [ 2 ] (69.2 km) portion over the Sierra Nevada remains unconstructed, and the California Department of Transportation (Caltrans) has no plans to build it through the ...
The California Historical Landmark reads: NO. 442 DEATH VALLEY GATEWAY - Through this natural gateway the Death Valley '49ers, more than 100 emigrants from the Middle West seeking a shortcut to gold fields of central California, entered Death Valley in December 1849. All suffered from thirst and starvation.
The crust in the Death Valley region between Lake Mead and the southern Sierra Nevada has been extended by as much as 150 miles (240 km). [18] The deep Death Valley basin is filled with sediment (light yellow) eroded from the surrounding mountains. Black lines show some of the major faults that formed the valley. (USGS image)