Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
(1) This zone if about 3 far of limestone is
decided an argillaceous limestone tending on
the the glaucites like magnesian and dolomitic.
There they lay around in St. J. P. P. but in the
magnesian layers it is hard to trace out the
forms. Fragments of Lingulae are common
done but draw no good ones.
(2) This difference dates included was not
one of dip but more probability is due to an
irregular erosion surface. To all intents the
beds of the entire section are horizontal.