Image from the Biodiversity Heritage Library.
Contributed by Smithsonian Institution Archives.
| www.biodiversitylibrary.org
Transcription
1000 Berea 7 AM.
87. J.C. Baker's farm, 3 mis of Ringtn,
970 ft. 8 AM.
5 mils of house.
No exposures at me here.
Siltfieldella bed. No fossils.
3'2" top of heavy layer at top of
7'ft massive Clinton limes.
Fault with Dermin on N
on same level as Clint, on S.
North of J.C. Baker house.
Strong plant toward SW,
Section not well expressed.
6'2" gray Derminian l.
1'ft limestone, weathering chalky, fish
layer, then, at top, At least wit
very small inodular material.
88. 1/2 mi. NE of New Liberty church
colored and 1/2 mil S of
Robtann store,
There is a layered section of soil
overlying the Black Slate
west of the road corners which
is probably the equivalent
to the clay at Jane's Grove
section, must be at this
layer only.
Derminian at junction of roads
and also 1/2 mi. W. reduced
to about 1/2 inch sandy layer
equivalent to fish layers,
90
89. N. of Dave Garrett's house at
N. end of Bobtann. Der. limestone
at least 4 feet thick, me sees as
five layers. Total not less now.
Exposure poor.
Fault here. Ordovician on
same level or north as Dermin
limestone on south of fault.
I made a mistake here.
In the well at Joe Creek Kump's
downse the Black Slate rests
or nearly directly in the Oford
beds that over intercedeiate
layers of Derminian were found.
Probably this is only a little
fish layer here and the rock at
Dave Garrett's is Clinton on,
1020 ft at 9.45 AM. The distance
from base of Clinton at Dave
Garrett's to base of Black Slate
at Joe Creek Kump's is 16'ft.
There may be a contact
cut right here. They weren't
13'ft below Black Slate
in well without reaching
massive Clinton.
at Mat Morris property,
honeers is Der. l. under
Black Slate & in shale.
Oxford clay below + Black
Slate about. Farther SE than
Der. l. is 14 mi. thick at crossing
wn stream.