Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
On the western side of the tracks of
Cairo just back of the return droil to
the west Ocoty Hyde showed me contact
between the Brindon and the "Leronian", One
is a magnesian Limestone the other a
fine grained hard limestone. All stand verti-
cally. Even though there is here a sudden
change in lithology I do not see why this change
should make the one Mississippi an the
other Leronian. I see no reason why both
should write Brindon, for certainly one
should look for something to represent the
elephant geor eny lamerite series of the
lower Brindon.