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[[stamped]] 0823 [[/stamped]]
[[encircled]] 16 [[/encircled]]

sandstone terminating in a coarse conglomerate. Above the cgl. is red, thinly cleaved shale like moccasin. This is followed by yellow, thin bed shale. Then comes more red ss up to the fault against the schist. (Pigeon) From about 0.1 - 0.15 miles E of US 411 to fault is mapped as Tellies but it seems to have the character of the Bays.

East of Benton just before entering gap in Sand Hills is Newala overlain by Lenoir with large Maclurites. This is overlain by 10 or 15' of cobbly ls with Bimmia 
[[left margin]] [[5 pointed star]] [[/left margin]]
Then comes shale. The shale east of Benton was determined by Ulrich as Athens. In the Arline tongue we saw Cystonotella, Leptellina and Orthomborides besides the Bimmia.

The Lenoir was not seen west of Cisco except for Mosheim. At Benton the Newala was followed by cgl. mudstone, yellowish in color Then came the Lenoir which seemed to be in a swale in the Newala. About 2 mi NE on this ridge at a road intersection a greater thickness of Arline appeared.