Field Notebook: Nova Scotia, Quebec, Vermont 1924, 1928, 1932, 1933
Page 263
Image from the Biodiversity Heritage Library. Contributed by Yale Peabody Museum of Natural History. | www.biodiversitylibrary.org
Transcription
Monday August 28-1933 Wea. THUR. SEPT. 16, 1909 Ther. Mine dol. louse occur further E to N. road. These I studied last year and the sequence E. is described quite as of August 19-1932 In the Parker Park drill. there are 2 real epyl. and dpl. including up to one foot acms. These an intraformational. Originally Howell was calling these Britt Rein and or came to the idea that all hidden in the sequence is of Hp.E. age. He puts it cell up. My anticline in Parker further east on the same road and described last year continues mine Parker east fn 400 feet, to the epyl. next to be described. At the eastern end of same road the Parker is overlain by a rug sandy dpl., above which is a rl. emply with thin slabs dpl. pieces and pieces of massive dpl that may be intraformational or one of the L.E. This makes the base of the Hp E. Then E. fn 150 feet is a sandy dol from 3'-5' thick with massive dol. Heads in it up to 16 nicks acms. Just at me the lcp dol. empyl occur the first horn-like prims. Further east about 50' is another shale ridge and it also has the horn-like prims. Have from pieces off it. Between the two emply is a real louse