Sandstone formations, Zion National Park

Référence de la vidéo 11940008
This rock alcove in Zion National Park in Utah is caused by the repeated freeze-thaw cycle of water that has seeped into rock cracks, a process referred to as frost wedging. Zion's monoliths are composed of nine distinct, exposed and uplifted layers of sediments which are part of the Grand Staircase, an immense sequence of sedimentary rock layers that stretches 200 kilometres from Bryce Canyon to the grand Canyon in the American Southwest. Here in Zion, the layers were laid down overt a 150 million year period before they were thrust upward by the forces of plate tectonics and carved by erosion. Famous for its spectacular scenery, the 24 kilometre-long valley attracts more than three million visitors from throughout the world each year.
Licence : Droits gérés
Crédit : Science Photo Library / Matulavich, Peter
Model Release : Non requis
Durée : 11 Secondes
Aspect ratio : 16/9
Restrictions : -

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