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[[stamped]] 0640 [[/stamped]] [[left margin]] 19. [[/left margin]] After seeing the Thorn Hill section we went down to Washburn and then over to Liberty Hills. At the bend of the road just before reaching the west end of the village occur Up. OHosee. Lower OHosee appears on the east side of the village along the highway about 3/4 mile. Here also occurred below the OHosee cherty ls. of the Lincolnshire. We returned to Thorn Hill and spent a short time at a cursory examination of the Evans Ferry section. At the base occurs a Mosheim lithology which is followed by red green mottled rock and this is succeeded by cherty limestone with Mimella and Dinorthis holdeni. This is followed by dark gray limestone with more scattered chert and big dinorthids. Above this just below the side road, occur cobbly shaly, yellow limestone with Strophomena mealeeri Dinorthis willardi and Multicostella (or Compulorthis). This horizon is not the OHosee but is the Strasburg as Ulrich contended. This is followed by a marble and then comes lower OHosee with Receptaculites. The Upper OHosee occurs by the large white house and consists of cobbly ls, and heavy beds of limestone with Camdaella, Hesper[[?]]this and Campulorthis. Around the bend to the south of the big white house is the so-called [[strikethrough]] att[[?]] [[/strikethrough]] Lowville as written of Cooper (B. N.)