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Association Round Table eroded valley. The present structure at the top of the J sandstone (stratigraphically older than the D sandstone) is a structural low in the area where D valley-fill sandstones occur. The trend and location of the low at J level are identical to the trend and location of the D valley-fill deposits. Thus, the present low at the J level confirms the paleostructure interpretation. This new model for D sandstone deposition, incorporating paleotopography and sea leveldoi:10.1306/ad461629-16f7-11d7-8645000102c1865d fatcat:kni543gvxvbabiuu4zygio3z2y