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The sea bottom shallows are 5500 feet above sea level at the magnificent White Pocket area of Vermillion Cliffs. Plesiosaur type swimming dinosaur tracks from the Cretaceous period can be found in abundance, petrified in the white sections of the ancient sea floor sediment. White foamed "breakers," waves made of stone and petrified in time, amid finned track ways and distinct tail grooves, small and large.
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