Rather, we infer that the Point of Rocks Sandstone was derived from erosion of . 'Quad Sandstone' at the Stanford University boneyard. the mineral separation lab. way by taking me out on a boat to photograph the coastal cliffs.
water depositional systems in arc-adjacent basins: the cretaceous-paleoge PDF
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Rather, we infer that the Point of Rocks Sandstone was derived from erosion of . 'Quad Sandstone' at the Stanford University boneyard. the mineral separation lab. way by taking me out on a boat to photograph the coastal cliffs.
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