Patricl cliff of dolomite if presunatly the Omallett. The crowed gone at its narrowest is not more than a few hundred feet across. In this crowded gone with faults that is a normal fault. To the east the Omallett is varied up repeating once or ten of the Omallett seems to the rocks. The drill to the north of the Oskahatin locality with forms [marked on topographic sheet @] has at least 250 feet of the deepest Omallett. Then at the school marked O on maps in the conglomerate with large boulders and some of them is also to be added. Therefore the Omallett is as follows: Opposite @ or near — 250 feet At School House ? 50 ft. The measured section 635-4 The actual thickness of Omallett is 935 ft or more.