Image from the Biodiversity Heritage Library.
Contributed by Smithsonian Institution Archives.
| www.biodiversitylibrary.org
Transcription
245
14
Going from 24 straight
Eastward: one of the branc
hs of Cedar Creek is crossed
exposing on the Eastern
side of the creek from 23
to 25 feet of Clinton ark,
weathering rusty brown.
Below it is the typical
Madism.
In the Clinton are
found:
-
Arthur flabella, good.
Arthur lyprata
strepomena thambi-
dalis.
Cgathrophyllum Day-
twhake.
Cgathrophyllum calycula.
246-
15
Quite a distance up the
stream, taking a right
hand fork, a great thick-
ness of Ozrord Clay.
Shale is seen. Perhaps
3 ½ to 4 ½ feet.
A clint distince SE
of the Ozrord Clay Expr-
sion in the creek bank
beneath a house, is
other exposure
151
above an old abandoned
house, a fine spring
is seen here issuing
from beneath a bluff
of 9 feet, presumably
D gravel rock, at
the upper edge of a brule.
the lower better stratified Conifermos.
247-
16
On the road from Cha-
pel Gap to Crab Orchard,
about 2 miles south of
Crab Orchard, the creek
bed east of the road
shows Black Shale rest-
ing on 6 ½ feet of dark
Brown Coniferuos at 1063.
248-
23 a
Just north of Crab Orchard
west of the Chapel Gap
road. The Black shale
rests on the dark brown
Conifermos at 1065.
-
Crab orchard RR 1078.
See the sections near Crab Orchard
for evidence that the Laurel
has probably not come in
yet.