Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
It is about 2 miles across from St. Armand
to Phillipstown, and age is Belmonton, lying at
low dips, about 10 to 20 degrees, to the E. or S.E.
Towards the railway there is some reversed dips and
here Logan has described a syncline.
This is the actual Champlain fault of Logan. With Cham-
plain fault in the next one east.