In all probability the top of Logan's Not. Where we started there were thick beds of conglomerate and no regularly bedded shales. Gradually the conglomerates became thinner and then sandstone with lints of granite boulders came in along with some regularly bedded shales, some of which have car- bmacerus and even one upright tree. Finally more and more shales were in the section. The fault at the south side of Apicus's Cove where an idea has a far greater throw than Josephson assumed by Fitcher. I will give surprised if it goes to 2000 feet and even more. In the carbmaceous shales of Apicus Cove I found rain imprints, Paur or Radiolites, Ostracods or Spirink's here. All of the beds seen today are evidently of fresh water origin. Some of the Pennylvanian must have crossed over the Cite guides. Possibly 4 did while divisions 2 and 1 of the rejuvenate Cite- guids represent the continental uplifts are seen at Panstron.