Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
July 14-1918, Sunday, Clam Cove.
This Sunday morning and we are taking things easy. Hitting of months yesterday and packing four small boxes of goods.
In the afternoon at 10 a.m. one went over from West Bay to climb Coney by the canyon road. The distance is 1/2 miles. We came to the shore practically vertical in a small pool (This turned out to be St. Dunman) is steeply standing high red soft coarse sandstone. At first the white ( = Lympus) These later found to be Indigosian stand with a dip of 620S,40E Farther north the Windsor shales are vertical and at 2 miles north by dip to the eastward. Found no faulting in this direction but later on found such near the brook.
The "Windsor" of the south horn of Clam Cove turned out to be Lower Permian.
Looking back to Clam Cove made the following sketch:
maybe 700' high
Do these a fault scarps?
Precipitous cliffs in places around hundred feet high.
These maybe of the Cow Head conglomerate.
Freelands probably 200 foot high.
Sea land
3 1/4 miles from mountain.
cliff
260
260
Continued
sea cliff
Further south headland.