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[[stamped]] 0631 [[/stamped]]
[[left margin]] 10 [[/left margin]]

and above Knox. It may be a swollen reef on the flanks of which Mosheim occurs.

Along the creek from the mill upstream shaly limestone with Christiania occurs. The Christiania is abundant in the soil on both sides of the creek. The Lenoir becomes more cobbly upward to the top where it is very cobbly. In the top occur many fossils Plestorthis and Multicostella plena occur about 75' below top. Large Opikina occurs at the top.

Above the Lenoir is Holston marble, shaly near top with Multicostella (Check with mine from 8 mi. WNW of London). Above Holston is Tellico and above Tellico is yellow sandy shale containing some marble beds and a specimen of Campylerthis. According to BNC this is upper OHossee. The Campylosthis was a biconvex type like some lower in the OHosee. Cooper (BN.) suggests that the cobbly upper Lenoir may be equal to Larber OHosee (possibly his Ward Cove, possibly the lowest Echinosphaerites beds.

The top Lenoir suggests the high Athens seen on the road SE of Sweetwater on Oct. 26. It looks as though the Lenoir completely replaces the Athens and the part replaced would be about the middle,