Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
"The Clinton appears the here with the same
and th[illegible]
character as at Hamilton. Belms are the thin bedded
about 8 feet, this is
limestones terminated above by the heavy bed of
at the Falls.
limestone which here is about 6 feet thick. Contact
Belms with the Oredina was not made out.
Did not see any Hyattella conjuncta said
to occur here (did not look hard for them).
The Archeatur is here easily mistaken
for the Lockport, Billings made out
thicker than at Hamilton.
6 to 7 feet. Suppose there is true but half the.
The Lockport here again has a
basal conglomerate as at Hamilton but
the opposite and sandstone was not made
out.
Cataract. At base in the Whilford sandstone
as at Hamilton followed by the same thin bedded
limestone series. Between 10 and 20 feet above the
sandstone occur the free A. Hancrocorae. This
is the type locality for the species.