Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Grimsby August 23-1912, Friday.
Left Toronto with Parks at 8 A.M. for Grimsby, Ontario which is 57 miles south of Toronto.
We climbed off the Cresta or 'Mountain' by the road back of the 'Village Inn' and up the new by the path on the north side of the run.
At the top of the Mountain occurs the Lock-
fjord dolomite that passes down into thin folded
magnesian limestone just as in the Niagara
force. Could not make out the thickness but
of lean folded dolomite
at least a foot once he seen in the cliff.
Then thin folded magnesian limestone without
shale cuttings pass into a transition of limestones
with some shales as at Niagara. Thickness
about 15 feet.
Then Rochester shale with thimble of
ajjadacene shale limestone refuse and forms.
These are the Rochester Shale, etc. as
may be seen of Niagara. Thickness about
30 feet. The fauna is identical with that
at Niagara Falls and Lockport.