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Big sky over the Devil's Golf Course in Death Valley National Park

Death Valley is the hottest and driest place in North America due to its lack of surface water and low relief. Thanks to the rainfall the valley received this year, you can see a shallow lake formed in Badwater Basin. This is an extremely rare event. People can even kayak in Death Valley although only temporarily.

Wrinkle, dry ground Badwater basin with mountains backround and blue sky in Death Valley national park in america at sunny day, usa

In the stark expanse of Death Valley, the Devils Golf Course unveils a surreal spectacle of vast salt formations and minerals that stretch endlessly. Against the backdrop of the majestic Telescope Mountains, this scene captivates with its barren beauty

The western sunset adds drama to other worldly salt formations at Devil's golf course, Death Valley National Park, USA

Devil's Golf Course in Death Valley National Park, California. A large salt pan on the floor of the valley.

View of Devil’s Golf Course in Death Valley National Park, California, United States. The area is covered with large salt formations that create a rugged and otherworldly landscape.

Dry flat salt landscape at the Badwater Basin at Death Valley National Park, California, USA. Seen a hot summer day.

Dry cracked earth in Salt Flats, Death Valley, NP, CA

$The Devil's Golf Course is a large salt pan on the floor of Badwater Basin located in the Mojave Desert within Death Valley National Park, California, USA. It was named after a line in the 1934 National Park Service guide book to Death Valley which stated that \$

Devil's Golf Course in Death Valley National Park, CA is one of the saltiest places on earth.

Captivating journey through the vast beauty of Death Valley's desert landscape. Explore the breathtaking Gower Gulch from the scenic hiking trail, framed by the majestic Telescope Mountains in the background

Devils golf course Death Valley salt clay formations National Park California

The crusty white deposits around Vixen Geyser’s vent are most likely mineral deposits, specifically silica and sulfate minerals. These deposits form when the hot water and steam from the geyser contain dissolved minerals. As the water cools upon reaching the surface and evaporates, the minerals are left behind, creating the characteristic white, crusty formations.

Image of Devils Golf Course in Death Valley detail of salt formations

Los Flamencos National Reserve. Area is made up of salt flats. The reserve is home to a variety of birds, including the Andean flamingo, Chilean flamingo.

Vast salt desert of Devil's Golf Course in Death Valley National Park. California, USA

Badwater Basin is the lowest point in North America at 282 feet below sea level. Periodic rainstorms flood the valley floor but soon evaporate because of the intense heat, leaving behind a pattern of crystals on the salt pan. Average annual rainfall in Badwater Basin is 1.9 inches a year. According to legend, Badwater gets its name from a mule that refused to drink the salty water. Badwater Basin is in Death Valley National Park, California, USA.

A vast salt pan featuring jagged and rugged salt formations, named for the idea that only the devil could play golf on such rough terrain.

Colourful sky at the basin of Death Valley National Park, California, USA. Seen at sunset.

Rugged salt formations of Devils Golf Course under a bright blue sky during daytime

Self-sedimented salt cracked in the heat of the sun in the desert in Death Valley, Death Valley National Park, California

Bad water basin in Death Valley national park, the lowest elevation in North America. At 282 feet below sea level another world landscape can be found. Visitors walk across the area next to salty water and mineral deposits in the stark but beautiful landscape.

Devil's Golf Course in Death Valley, California

Landscapes of the Atacama Desert

travel in USA

$The Devil's Golf Course is a large salt pan on the floor of Badwater Basin located in the Mojave Desert within Death Valley National Park, California, USA. It was named after a line in the 1934 National Park Service guide book to Death Valley which stated that \$

Mineral deposits on desert floor Death Valley

The crusty white deposits around Vixen Geyser’s vent are most likely mineral deposits, specifically silica and sulfate minerals. These deposits form when the hot water and steam from the geyser contain dissolved minerals. As the water cools upon reaching the surface and evaporates, the minerals are left behind, creating the characteristic white, crusty formations.

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