Bryce Canyon National Park
Lees Ferry, Arizona), White (which surround Utah Zion Canyon), Gray and Pink. Most of the Grand Staircase is now contained within the BLM-managed Grand Staircase - Escalante National Monument. The rocks that give Bryce Canyon its distinctive colors are members of the Claron Formation, a mixed Highlights limestone/sandstone layer, and are also found exposed, with similarly intricate forms, in other nearly locations such as Red Canyon and Cedar Breaks. Erosion: Water is responsible for creating the rock shapes in Bryce Canyon National Park. Rain and melting snow flowing down the Pink Cliffs towards the Paria River form ridges, or fins, which subsequently erode into the spires, pinnacles and other shapes (collectively known as ‘hoodoos’) which are left standing. In time these too erode, and the whole process moves very gradually westwards as more of the cliff is slowly worn away. During the long, cold winters, the cliffs are further weakened by freezing water Bryce Canyon National Park expanding in cracks, resulting in more erosion when the ice Bryce Canyon National Park does not contain one main thaws in spring. canyon, but rather a dozen smaller ravines eroded into the east side of a ridge running approximately north-south at Bryce Canyon Trails: As with most national parks, the best the edge of the Paunsaugunt Plateau in southwest Utah. This way to appreciate Bryce Canyon is to explore away from erosion has resulted in thousands of bizarre and fragile rock the main roads. There are various trails both along the rim formations, large and small, in many subtle shades of pink, and down through the formations, but probably the best white, yellow, orange and red, extending in quite a narrow is the Fairyland Loop Trail, an 8 mile, little-used route which band for over 25 miles along the plateau rim.
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