Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
In general we could call these brown white
sandstone, whilst red but this can be done only on
the basis of color and position. There is certainly
no Cataract run it in the red shale above have
the agulotins Medenia fauna.
The brown 8-10 feet of the white sandstone
are amid erms bedded,
Other fossils than Orthothycus are
very scarce, but but we find [illegible] and
no Lepudilia,
In the red beds shale conglomerate is
common. In a case of sea churning, the pebbles
may be as large as 2 inches across. They are
always flat when large, but those if little bits
are often more rounded.