Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Our my muddy roads are more slow
and hard driving to get to Grey Creek, but
it rained all afternoon and we concluded
not to try. After much labor with the car
and engine we reach at 5.30 Dunfermline
when we put up in the night.
Morgan tells me that on the north side
there are many limestone conglomerates,
and that these
usually called the Trogos
often traced around are seen to interfinger into
various levels of the Boggys. Furthermore as
we approaches the close of the Pennsylvania
whose groups appear made up of large field-
morgan calls the Porttatoe conglomerate, and
opens. These conglomerates and arkoses can
make head more than 40 miles out from
the Cathneels mountains. The evidence appears
to be that the limestones and finally the arkose
is derived from an Athneelle dome in Penn-
sylvania time. That the limestone bodies
fall signs up to 6 miles across could not
have been transported hundreds of miles in