Owens Valley / Alabama Hills
Many of these stand on end due to spheroidal weathering acting upon nearly-vertical joints in the rock. While the rocks of "Alabama Hills" are identical in composition to the 14,000-foot peaks looming above, the difference in appearance is the result of the weathering processes. Up high, the freezing snow has caused the splintering of the granite seen at Mount Whitney. Down in the warmer Owens Valley, the "Alabamas" took shape when the climate became drier, exposing and shaping the piles of boulders. Water and wind continue to shape the landscape and rocks to this very day. The beige and blacks in the mottled coloring are the result of being stained for millions of years by the oxidation of the iron minerals in the rock. - Jennifer
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