Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Jvte
The hills here are not high, probably not over
200 ft above low water mark and flat toped.
There are far side valleys or that the county
above the river valley make the flat a slightly
undulating and at for pulled as at Cinte.
Elkhorn Creek 1m. south of
Richmond.
Overlying Clinton Corridal
limestone. Rocks down
and slides over the
shale below.
a greenish (clay) shale
cracking down to clay,
4 feet.
Clinton Lake.
This disconformity appears
to be a very even surface.
Tof of Richmond. Fossils
mostly bygros and Helbertella
sinuata.
creek at low water