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This sand is from the Big Sur coast of California, with many metamorphic rocks created near an ancient subduction zone. The sand on the right is 100% composed on shells, coral skeleton, and other biological precipitates.
Wind carried sediment falls to the ground when the wind slows down. Deposits formed by wind erosion and deposition include sand dunes and loess deposits. Sand dunes have coarse grained sediments, loess has finer sediments, both are caused by wind erosion.