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The hoodoos at Bryce Canyon experience more than 200 freeze-thaw cycles each year. In the winter, melting snow, in the form of water, seeps into the cracks and then freezes at night. When water freezes, it expands by almost 10%, prying open the cracks bit by bit, making them even wider, similar to the way a pothole forms in a paved road.
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The park is located in southwestern Utah about 50 miles (80 km) northeast of and 1,000 feet (300 m) higher than Zion National Park. [6] [7]Bryce Canyon National Park lies within the Colorado Plateau geographic province of North America and straddles the southeastern edge of the Paunsaugunt Plateau west of Paunsaugunt Faults (Paunsaugunt is Paiute for "home of the beaver"). [8]
Bryce Canyon is famous for “otherwordly” rock formations known as hoodoos — “spires and towers that appear as forests of rock,” according to the U.S. Geological Survey. Hoodoo pillars ...
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Goblin Valley State Park and Bryce Canyon National Park, also in Utah about 190 miles (310 km) to the southwest, contain some of the largest occurrences of hoodoos in the world. The park lies within the San Rafael Desert on the southeastern edge of the San Rafael Swell, north of the Henry Mountains.
Wikipedia: Featured picture candidates/Image:USA 10654 Bryce Canyon Luca Galuzzi 2007.jpg
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