1971  Gordon: C40: lower part of Chainman Shale with
           Entogonites borealis at its base, several beds with
           Goniatites americanus, middle part with Goniatites
           multiliratus, upper part with Dombarites choctawensis.
           
           SE1/4NW1/4 and NE1/4SW1/4sec.7, T.14 S.,R.17 W., on
           the northeast slope of Granite Mountain, Utah, showing
           the succession of goniatite-bearing beds.