The Appealinna Well lead prospect is situated on the northern limb of an east-west synclinal structure within calcareous siltstones, shales and dolomite lenses of the Konoka Formation. Lead minerals occur as small lenses and pods within narrow quartz-calcite-siderite veins crosscutting and paralleling bedding of the enclosing sediments. It is unlikely that any of these would prove economic. No further exploration is warranted