Apparently a lot of car companies come here to test drive new vehicles. There is no test track as such, but the varied terrain and dramatic change in temperature and altitude are perfect to try out engines and breaks.
Mt Whitney, the highest point in ‘the lower 48 states’ is less than 100 miles from Badwater Basin – elevation -282feet and the lowest point in North America. The temperature changes 5°C for every 1,000 feet, and there are three ranges of approximately 10,000 feet and two valleys of searing hot temperatures within the park, which would certainly create some challenging driving conditions.
The wind is ferocious at Ryolite, an old ghost town. When gold was discovered in the early 1900s, 10,000 people flocked here – three railroads and many buildings emerged, including casinos and a three-storey bank. The boom went bust as the price of gold fell through the floor and the ensuing panic ended the gold rush by 1912. Now the town is eerie with the sound of bits of bank and casino flapping and whistling in the wind, and signs by dilapidated stores caution ‘Rattlesnakes’.
Old pictures show the mines and mule trains – this area is certainly rich in minerals and was ripe for exploitation until Congress passed the Mining in Parks Act in 1976, which restricted and regulated mining in Death Valley for the first time. The park is now closed to new mining claims, and previously established claims and mines are closely monitored.
The colours at Zabriskie Point, and indeed everywhere, must change hourly and would be worth photographing throughout the day. This is a crazy place full of geological treasures.
The National Park brochure claims, ‘The colourful and rugged terrain shouts tales of cataclysmic forces that thrust thick rock layers upwards and of opposing erosional forces battling to tear them down. Desert winds whisper romances of the past – of the ’49ers lured by the glitter of gold and of Chinese labourers scraping borax-rich crystals from the valley floor.'From Dante’s View, the mineral deposits in the mountains are the colours of the Firenze cathedral’s marble walls. Rivers of salt run down the valley.
At Badwater Basin, below sea level, salt flats stretch for miles; their crusty layers look like a particularly unappetizing meringue or Kendal mint cake.
Strange miniature pinnacles dot the Devil’s Golf Course and cairns are made from slabs of salt.
The artist’s palette features mounds and bands of many hues, as though the artist has dumped all his colour and pigments into one vivid lump. The residue of the excavated minerals leaves colourful rainbows on the land.
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