Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
"part of the Limestone limestone =
Clark Mills beds unquestionably
To Silurian aspect. On the other hand
there appears little no break between the
Limestone ls and the Stormville shale
and yet the two faunas are wholly different.
some condition affected the life of this
uppermost Silurian sea wiping out as a
rule the limestone and fauna and
beginning a new cycle with chert and
shaly Cherts with chert with a fauna a
migrant since it is not a development
out of the Siluria one.
May 31- 1901 Friday
Delinopore Junction 5 m. below
Cumbury.
Left Stormsburg at 8.44 and
arrived at the Junction at 10.10. Rallied
north 7 miles to show this very complete
section regions.
Crest of hill
Soil 10'