Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
"Continued from
page.
From this
point of the chalky layer,
are more evenly layered
and almost devoid of casts
especially Favositae!
12'
4'
5'
45'
2'
38"
Recently formed shales
S. shemardi bed. 4ft.
Another Favositae bed. Cocks not
or perhaps as below.
Shales with zones of gastropods,
cleefords and Trigonia? These
are scattered throughout but are
only abundant at the middle
and base.
Limestone
Ordnite.
< du fruits, S. shemardi bed.
< Min furcation here one
frid.
< 18 ft above mou frid.
< 36 ft above base many fossils,
like that fig 11 in this place.
Also two fine Trigonia's come from here
Ordnite beds might have life
< One problem the limestone seems gass. but its
Cocks along had here for 450 yards, Shale
can be seen of lower Hils for 30 yards.
I have no doubts that the shales are in
due up to the Ordovite, 120 yards beyond
the 240 yard place where Cocks are still
present."