Field Notebook: Nova Scotia, Quebec, Vermont 1924, 1928, 1932, 1933
Page 256
Image from the Biodiversity Heritage Library. Contributed by Yale Peabody Museum of Natural History. | www.biodiversitylibrary.org
Transcription
Wea. THUR. SEPT. 9, 1909 Ther. Later concluded that this cycl. is due to ea. frost sliding. The trees are too irregularly deforested at me and somewhat help to be a depositional cycl. These forms turned out to be uppermost Parkers, sit around Olencides.