Fast uplift of a mountain range in an arid environment often does not allow its canyons enough time to cut a classic V-shape all the way down to the stream bed.

Instead, a V-shape ends at a slot canyon halfway down, forming a 'wine glass canyon.' Sediment is deposited on a small and steep alluvial fan.

Approximately 95% of the park is a designated wilderness area.

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The second-lowest point in the Western Hemisphere is in Badwater Basin, which is 282 feet (86 m) below sea level.

The park is home to many species of plants and animals that have adapted to this harsh desert environment.

Death Valley National Park is a national park in the United States.

Straddling the border of California and Nevada, located east of the Sierra Nevada, it occupies an interface zone between the arid Great Basin and Mojave deserts in the United States.

There are two major valleys in the park, Death Valley and Panamint Valley.

Both of these valleys were formed within the last few million years and both are bounded by north–south-trending mountain ranges.These and adjacent valleys follow the general trend of Basin and Range topography with one modification: there are parallel strike-slip faults that perpendicularly bound the central extent of Death Valley.The result of this shearing action is additional extension in the central part of Death Valley which causes a slight widening and more subsidence there.A group of European-Americans that became stuck in the valley in 1849 while looking for a shortcut to the gold fields of California gave the valley its name, even though only one of their group died there.Several short-lived boom towns sprang up during the late 19th and early 20th centuries to mine gold and silver.This uplifted the region out of the sea and created a line of volcanoes.