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Crossbedding
in Zion National Park
Photographs by Jimmie D. Agnew

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Crossbedding
occurs when deposits accumulate from wind or water that changes direction.
In streams, crossbedding results when streams change course. For wind
deposited sediments, sand accumulates at different angles when the predominant
direction of the wind changes. In Zion National Park, evidence of the
changing direction of the wind is preserved in these fossilized sand
dunes. Various angles of deposition are evidence of wind's coming from
different directions.
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