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[[stamped]] 0692 [[/stamped]]
[[left margin encircled]] 34 [[/left margin encircled]] 

On way to Pulaski stopped at Sharon Sprs. locality to collect [[strikethrough]] ion [[/strikethrough]] silicified fossils. Overlying the Athens-like cobbly beds occur calcarenite and cobbly ls. with Dystactospongia, rare Stromatocerium which suggest Wardell. Cooper has already called them Belbolt. Above these occurs Moccasin.

November 5 -
Breakfast                          [[strikethrough]] 1.20 [[/strikethrough]]
Lunch                              [[strikethrough]] 1.20 [[/strikethrough]]
Supper                             [[strikethrough]] 2.51 [[/strikethrough]]
Hotel, Pulaski                                       3.50
Cabin at Christiansburg                              3.50

At Quarryville we looked at the abandoned quarry near its east end. Here the ls. rock under the shale is coarse, thin to heavy-bedded calcarenite and undoubtedly is Holston. Beds of "Up. Lenoir" type were seen intercalated in the lower part of the sequence. Some of the quarry beds are a mass of small bryozoa. Evidently Butts identified Lenoir under the black shale at the west end of the quarry. The quarry rock at the end we investigated is most certainly Holston.

Early morning went to Draper, Virginia where, on the Lecanospira zone of the Canadian occurs a chert conglomerate in the base of the middle Ordovician,[[guess]] This is followed by about 100' of