Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
In other places this shale has been
removed by the glacier since none
about the rock is striated and worn
by drift. In this shale I found
nine dolatopirinae and the bygon
remind of the Partidge Point one.
This then prove that the Partidge Point
beds also occur in Phelps quarry
overlying the # Geerowlaya beds. It
is below there that the spirifer grand-
liferae beds of Thunder Bay more
occur. The following is an ideal
section:
Oct. 9.
A
Partidge Point bed
13 feet
B
Partidge Point beds (variet) seen 5 feet.
and Stromatopor
Phelps quarry, Accumulation beds. These
regular bedded about 7 ft thick; in the down
it is not less than 20 feet thick.
T. B. F. section for
in line.
Hiatuse not known. Probably but a few feet.
C.
Thunder Bay river shale beds and A. grandifera
seen about 5 feet.
This bedded limestone bed. In fossiliferous
with shale partings
seen about 7 feet.
Prie.