Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
"Still far the west of Trappus Cove we came up m 2
and smelled elevate rocks on at 15' with a cliff 20' high
back of it. At 40 far above the sea the land is level
smelling the second beach. These beaches are in glacial
material (to me looks like onoramic). This glacial material
continues all the way to Whale Bay and in all this distance
there are no Cidnoric outcrops. Also saw Orga arenaria in them.
At four half miles east of Whale Bay from the opening to
Large Pond) Onoritic rock exposures again occur. It is a
decay bedded dove colored, mottled with white, onepression lines.
two (granite or limestone) having some silicous footprints of
which are hole out all their own good and accessible. These
look more like those of 8 that of any other horizon. In the
present we think the horizon are &. See the books,
our course or one part of whale bay area we came upon
another settlement and here again we saw nothing more than glacial
(onoramic) material. One of the inhabitants told us that the
same kind of material occurred all the way to sea Fontaine
Point. We therefrom took the skater path cut through the woods,
"The Government Road" and on five miles or more among
the mosquitoes and over the stumps on a hot day, Tomahfel thinks
honestly the saw entirely in this distance from Bruce Bay.
We came out of the woods at Ballen and from here to
Table Point we walked over "the barriers" and the coast is all
glacial material to about five miles east of the Point. See
Tomahfel reports give 9.
At Whale Bay the strike is N170E, dip 4 S.
Five mile east of Table Point the general strike goes pm