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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]
An unimproved road through Amargosa Valley, connecting Nevada to Death Valley Junction, appears on state maps as early as 1927. This route crossed the state line roughly where the current highway crosses now, but instead veered northwest to State Route 5 (now US 95) southwest of Beatty near the now defunct town of Caracca. [3]
State Route 374 (SR 374) is a state highway in Nye County, Nevada, United States. It serves as Nevada's gateway to Death Valley National Park, connecting the park to Beatty. The highway was known as State Route 58 prior to 1976.
State Route 372 (SR 372) is a short state highway in Nye County, Nevada, United States. The route connects the town of Pahrump to the southeast side of Death Valley National Park via California State Route 178. The route was formerly a part of State Route 52 until being renumbered in 1976.
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]
By 1907, about 4,000 people lived in Rhyolite, according to Richard E. Lingenfelter in Death Valley & the Amargosa: A Land of Illusion. [34] Russell R. Elliott cites an estimated population of 5,000 in 1907–08 in Nevada's Twentieth-Century Mining Boom, noting that "accurate population figures during the boom are impossible to obtain". [35]
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.
Devils Hole is a geothermal pool within a limestone cavern in the Amargosa Desert in the Amargosa Valley of Nevada, east over the Amargosa Range and Funeral Mountains from Death Valley. It is at an elevation of 730 m (2,400 ft) above sea level [3] and the water is a constant temperature of 33 °C (91 °F). [4]
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