Image from the Biodiversity Heritage Library.
Contributed by Smithsonian Institution Archives.
| www.biodiversitylibrary.org
Transcription
29
29) North of Floyd's Fork. Hays Spring.
2 2/3 ft Clay. Upper Ozgood.
5 1/2 ft Ozgood limestone.
21 ft. Thick Ozgood clay. Some indurated layers at top
1 1/2 ft Transition rock See page 8.
15 in. Salmon brown Clinton.
{Fairly hard just below Clinton,
25 ft {Madison -- weathered to thin bedded stuff. (No gasteropod bed at top)
3 ft More like banded Madison.
8 ft. Clay rock spalling in all directions.
2 1/2 ft Soft clay.
{2-3 in. Limestone with
Strophomena plamumbma
Streptelasma rusticum
Rhynchothema capax
The rocks next mentioned consists
chiefly of small limestone rubble. Very
little limestone in hard layers.
5 1/2 ft
5 1/2 ft Strophomena plamumbma at base
5 1/2 ft Protasoa retusta common
Streplasma planumblma common
11 ft Protasea retusta at top
0 -- Streptelasma rusticum = 6.6 ft
below Clinton.
1 ft. Soft dark blue clay.
0 ft Columnaria balli? with conallite
separate at top as as to leave
separate epithica.
9 ft. Soft clay limestone. Soft clay. Fossils.
31 ft. Fairly solid limestone. With very few fossils
3 in. Coarse coal. pebbles = 3 in.
That part of the section below the double line
was recorded at locality = 30