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  2. Geology of the Death Valley area - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Death...

    Little is known about the history of the oldest exposed rocks in the area due to extensive metamorphism.This somber, gray, almost featureless crystalline complex is composed of originally sedimentary and igneous rocks with large quantities of quartz and feldspar mixed in. [1] The original rocks were transformed to contorted schist and gneiss, making their original parentage almost unrecognizable.

  3. Racetrack Playa - Wikipedia

    en.wikipedia.org/wiki/Racetrack_Playa

    Since their first description in 1948, large rocks up to 320 kg have been seen being moved across Racetrack Playa in Death Valley, leaving unique paths in their wake. The physics of this rock movement, thought to be caused by wind on a wet and slick playa surface, has been a matter of continued discussion for years despite the observation of ...

  4. Ubehebe Crater - Wikipedia

    en.wikipedia.org/wiki/Ubehebe_Crater

    Ubehebe Crater in Springtime. Geologists call the resulting large steam explosions hydrovolcanic or phreatic eruption and the pits created are known as maars.Ubehebe was the last and largest in a series of similar eruptions in the immediate area (its eruption exceeded the tensile strength of the bedrock by 10 times).

  5. Sailing stones - Wikipedia

    en.wikipedia.org/wiki/Sailing_stones

    Sailing stones (also called sliding rocks, walking rocks, rolling stones, and moving rocks) are part of the geological phenomenon in which rocks move and inscribe long tracks along a smooth valley floor without animal intervention. The movement of the rocks occurs when large, thin sheets of ice floating on an ephemeral winter pond move and ...

  6. Ubehebe Craters - Wikipedia

    en.wikipedia.org/wiki/Ubehebe_Craters

    The Ubehebe Craters are a volcanic field in the northern Death Valley of California, consisting of 14–16 craters in a 3-square-kilometre (1.2 sq mi) area. The largest of the craters is the 800 metres (2,600 ft) wide and 235 metres (771 ft) deep Ubehebe Crater.

  7. The Grandstand - Wikipedia

    en.wikipedia.org/wiki/The_Grandstand

    As with the rest of Death Valley National Park, The Racetrack and The Grandstand receive very scant rainfall, rarely more than 2 inches in most years. Due to its elevation of 3,000-foot (910 m), the climate at The Grandstand averages slightly cooler than that of the floor of Death Valley; however, daytime high temperatures are commonly above ...

  8. Why is Death Valley one of the hottest places on Earth? - AOL

    www.aol.com/why-death-valley-one-hottest...

    Here’s what we know about the valley dubbed as one of the hottest places on Earth. In 2022, over 1 million people visited the national park. Here’s what we know about the valley dubbed as one ...

  9. Titus Canyon - Wikipedia

    en.wikipedia.org/wiki/Titus_Canyon

    Titus Canyon Road, with view of Death Valley. Titus Canyon is a deep, narrow gorge cut into the steep face of the Grapevine Mountains of the Mojave Desert, within Death Valley National Park in southeastern California and southwestern Nevada. The canyon features limestone rock formations, petroglyphs, and native plants and wildlife. [1] [2]