Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Near the middle of the Trenton, at the footfalls
of Rocky Brook we again saw distinct beds, but far
or thay at Taylor Tally.
Late along with large Orthoceras, Trachymera,
Raphistoma. Hydra appear rarely Cyclaspis
fisulenta. Labor thought down the Frankfurt by Orthos
reminding of O. gracile. Onerosus reams rough
In the afternoon rode about four miles east
to Weststone brook to see the Utica and the
higher Cincinnati series. The Utica is the
normal Haell shale with some large Treachters
feeli n large specimens. Endromus juteiforme is
abundant. Inaptiles are rarely seen and other
forms. These Haell shales fans into green gritty
sandy shales that hidden of introduce more and more
thin sandstones (from 1/2 to 2 inches thick) and more
thinner than is a persistent sandstone some, all in shale.
nearly thin sandy limestone in the latter abound in Bygon
dolmanella, or large Plectan trills, rarely Ru-
also Contrita. And two
Phragma alternata, Gygopina cincinnatensis.
In the thin sandstones the same forms occur but
more often Dolmanella, Plectan trills, Byssomychia
radiata, Orditepisis modistaris and other smaller
forms. Also saw little Cornulites (always simple)
or Tentaculits. Saw me Scrovinus subcrassus
and jukely Eotemronius. Splytremains columnals are