Field Notebook: Bermuda, New Brunswick, Quebec, Vermont 1929
Page 69
Image from the Biodiversity Heritage Library. Contributed by Yale Peabody Museum of Natural History. | www.biodiversitylibrary.org
Transcription
Jacquet Riou, July 18, 1929 (continued) We must be able to overtop the great Turgen horizon and bore east, for which at least two-thirds is a sign of success that Alcora thinks looks like what he really believes in flora. If we try any path with it. See unimportantly. The Turgen is plainly overlying the horizontal Bonaventure and in places fills hollows in the Turgen. This angle, from our work for a long distance, to a little dead end employed by Lara flora. Then to us, more angle, and then a very thin line flora. Together they must be here 2000' of Turgen angle or even more. We then continued south to Turgen R.R. station, and half-way back came upon a Lilian exposure of young "Bella clune formation". The ds stand near on edge and other beds has been disturbed away it leaves behind semi-siliceous fossils the most interesting of which are small and very large Palaeocycalus mist. Other fossils are cupenae, Ortha, Flabellites. Fossils are scarce. The design appears to be about higher Clenoile or even La Vielle. We then continued east across Hendry Brook to see the Elm tree slate, but instead encountered the dead angle, as seen yesterday in the intersection of R.R. road. Further east one came upon an apillite suggesting the Leptocaelia flabellites beds seen yesterday. Accordingly the Elm Tree formation is new.