Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
"got in from the once spedy marine creatures but
did not succeed in getting a foothold.
Outside of a population marine fauna
through a long thinness
is at hand, though the fossils are never common.
Just before the Catskills condition is permanent,
yet hand we got specific oreocratalis and
smalle hippy-ellermani-
a brannysia. This design seems to be about.
The fossils always drift out in approaching
the red beds. In the red beds one always sees
sun-croeting, rain imprints, rill markings
and in one place we saw fossil foot prints.
Also foot markings are common in the red
muds and even in the red muddy sandstones.
We then go through several thousand feet
of greenish sandstones with zones of red shales
are of different Dermin age. Throughout lower
gets the Archaeopterus flora. Our marine
fossils are to be seen. The sandstones often have
imprints of stems of coral of 1 to 2 inches in
diameter. Sometimes they are conglomerates of
green shales, bottles,
river action tearing up the muds