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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.
The dunes shown in this image are advancing toward the northeast, and the brilliant white sands contrast with darker soils. The sands of White Sands National Monument are formed from gypsum, a soft mineral often left behind when water bodies evaporate.Although gypsum is a fairly common mineral, it is rarely found as sand because it easily dissolves in water, and rivers generally carry dissolved gypsum to the sea.Waters flowing into the basin holding White Sands National Monument, however, found no outlet and evaporated.lthough gypsum is a fairly common mineral, it is rarely found as sand because it easily dissolves in water, and rivers generally carry dissolved gypsum to the sea. Waters flowing into the basin holding White Sands National Monument, however, found no outlet and evaporated.