| http://www.w3.org/ns/prov#value | - The basis for such recognition has been, besides the gross lithology noted above, the different combinations of lesser Kokomo lithologies that consist of intraformational breccias and contorted beds (considered to represent soft-sediment deformation), algal stromatolites, cut-and-fill structures, molds of evaporate crystals, and other features generally ascribed to very shallow subtidal to intrati
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