Why Death Valley National Park
Death Valley National Park lies along the California–Nevada border, east of the Sierra Nevada mountains. Spanning Death Valley, portions of Panamint and Eureka Valleys, and most of Saline Valley, it is the largest national park in the contiguous United States and the fifth largest overall. The park serves as a transition zone between the Great Basin and Mojave deserts, encompassing salt flats, sand dunes, canyons, badlands, and mountain ranges. Over 93 percent of its area is designated wilderness, and in 1984 it became the core of UNESCO's Mojave and Colorado Deserts Biosphere Reserve.
The landscape features extreme changes in elevation. Badwater Basin sits on the valley floor at 282 feet below sea level, forming the lowest point in North America and the second-lowest in the Western Hemisphere. This area features one of the world's largest salt pans, rich in borax and salts, as well as notable natural sites like the Racetrack playa, known for its sliding stones. Surrounding mountains, including the Panamint Range crowned by Telescope Peak at 11,049 feet, create dramatic topographic relief. Despite the arid environment, adapted wildlife and flora flourish, such as bighorn sheep, coyotes, Joshua trees, creosote bushes, and the rare Death Valley pupfish.
Indigenous groups have lived in the area for thousands of years, most recently the Timbisha, who historically migrated seasonally between valley winter sites and mountain summer grounds. European-American travelers searching for a shortcut during the 1849 Gold Rush named the valley after becoming trapped there. Later, boom towns appeared during brief gold, silver, and borax mining eras, the latter transported by famous twenty-mule teams. Resort development in the 1920s around Furnace Creek and Stovepipe Wells spurred tourism. Designated a national monument in 1933, the area expanded to national park status in 1994 and became a designated dark sky park in 2013.
Death Valley is recognized as North America's hottest and driest location due to a strong rain shadow effect caused by surrounding mountain ranges. Summer daily high temperatures frequently exceed 120 degrees Fahrenheit, with the highest reliable air temperature ever recorded on Earth—134 degrees Fahrenheit—measured here in July 1913. Winters bring cooler days and occasionally freezing nights. Rainfall is extremely sparse, averaging about 1.5 inches annually at Badwater, though rare heavy downpours can trigger intense flash floods across the desert basin.
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