Viewing page 214 of 473

This transcription has been completed. Contact us with corrections.

[[stamped]] 0637 [[/stamped]]
[[left margin]] 16 [[/left margin]]

Cryptophragmus. Across the brook in the bluff occur thin-bedded limestones with shaly partings and abounding in Rosticellula and bryozoa. Opikifa[[guess]] is also present. Above the rhynchonellid beds occur Moccasin reds.

Along next NW road to the NE the blocky chert, red, mealy rock, Lincolnshire-like limestone and OHosee lithology occur.

Old Road extending NW for 1/2 mile and located 1/2 mile SW of the Fleanor Mill showed a wonderful section. The blocky chert occurs 245 paces NW of house and is overlain by red shaly rock. 132 paces SE from first stream & road crossing occur Oligorhynchia in a thin ls bed. Mimella is also present. This bed is located about 475 feet NW of the house. The Ologorhynchia bed in the red are layers of hard fine-grained sandstone, and calcareous shale, the latter with many Strophomena (suggesting measleri). In the sandstones occurred Dinorthis willardi and a possible Sowerbyites. Following these beds and on the south side of the small creek near the house occur the cherty, dark limestones with Bryoaoz. At the intersection of the old road and main NE - SW road and for 25 yards NW occur cobbly shale and limestone with Lower OHosee fossils. According to Cooper (B.N.) this is the real lower OHosee, the Sowerbyites beds are not OHosee at all