Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
This one is like other Clinton we only have there is more frag-
mental material, some sand and bone white, fossils occur. It
does not lie at the base of the dolerite but 3 feet above the base
of these formations. The rim one is decidedly cross-hilled.
It is made of a crystallized material, bygone, Tenta-
culites, some sand, and certain rolled fragments of
iron all superimposed and erected inside him.
The layers below and the one hand show crone marks
= undulating or waves.