Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
August, Tuesday, 7. Perryville.
Packed on two boxes and shipped them at Camden. Left at 9:58 A.M., and left for Perryville via Hollow Rock and Lexington. Arrived at 6:30 P.M. after a walk of 4½ hours at Lexington.
2947
August 8, Thursday, Perryville.
Was up at 5:30 and away at 6:15 in the quarry near operation about ¾ miles north of the village.
Here may be seen the top 20 feet of the Browns-peak upon which rests without apparent break the New Zealand. It begins with a limestone member probably 5 to 8 feet thick, a crinoidal limestone having an abundance of Mariacrinus stenius and an occasional Camarocrinus. These same beds also have the regular New Zealand fauna for in it I saw Stenijus magnificus, S. pelamella, Stricklandia beechi, Meristella atrica, and striatipora.
These limestones are followed by blue shales that weather out as a tough sticky clay full of fossils of the New Zealand type. Only one animal comes from these shales, here appear the first Brycidula and Michelinia.
Above is a debris of Camden shale mixed with sand at some of the [illegible] Luderburge clay. It in clay.