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The geology of the region (the Grand Staircase)
Illustration by Darlece Cleveland Bryce Canyon: The Desert's Hoodoo Heart by Greer Chesher |
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The term "Grand Staircase" refers to a sequence of sedimentary rock layers that form a massive "staircase" between Bryce Canyon and Grand Canyon. Each canyon's cliff edge acts as a giant step displaying the earth's geologic history and its layers. As one moves down the geologic column, each successive rock layer is older than the previous one. The oldest exposed formation in Bryce Canyon is the youngest remaining layer in Zion Canyon. Likewise, the floor of Zion Canyon is Kaibab Formation, which is the same formation one stands on at the Grand Canyon's rim. As one stands at the South Rim looking into the depths of the grandest canyon of them all, one is witnessing some 2 billion years of geologic history.
Your Guide to the National Parks by Michael J. Oswald |
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We could not visit Zion in the morning because a storm caused mudslides, and a large boulder rolled onto the entrance road. We returned before the sunset and had only a few hours before it grew dark. This page does not do justice to this beautiful park. We will be back.
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The road to Zion National Park is closed
August 11, 2016: 5:36 AM |
Returning to Zion National Park
August 11, 2016: 4:57 PM |
A mule deer (Odocoileus hemionus) in Springdale, Utah
August 11, 2016 |
We have finally arrived!
August 11, 2016: 5:27 PM |
The North Fork of the Virgin River
August 11, 2016: 5:33 PM |
The moon over the cliffs (waiting for the shuttle)
August 11, 2016: 5:34 PM |
Cliffs
August 11, 2016 |
The sunset
August 11, 2016 |
Weeping Rock
August 11, 2016 |