Image from the Biodiversity Heritage Library.
Contributed by Smithsonian Institution Archives.
| www.biodiversitylibrary.org
Transcription
171. Cauderill at 875 as well as
can be made out from
residual material and for
entire lines.
Grand Switch.
At creek 1 mi NW Grand Switch &
thin bedded with layers, from top on,
Partially the not thin bed, since the
sample is confined to massive,
but it may be the strip are of the
same. No diagnostic fossils noticed.
Stephensona in upper Lewis verno between
line and half way from Creek to Gran
del Switch.
179 old number! Hardly long a mile
NW Grand Switch at the forks of
the road, the stream bed exposes clay
rock, spalling into small fragments,
with Plate ponderosa &,
13 feet above this level is the design
fully Brachypora and modular
masses, same as Sy Raneland
at Rileys.
Permian limestone occurs a short dis-
tance at or the level, both NW of creek
presently rest more than 10 or 15 ft
higher. Black shale stone,
About 1 mi SW Grand Switch where road
crosses Creek, going west, and thus passes,
Dec 6, only 4 & 2/3 mi a distance exposed.
25 ft interval.
Lugia + Brachypora + ms Aulac Canny.
Still more down stream the drove
entered limestone comes in at least
16 ft below the Brachypora layer. Pass
the mine.
At North Fork nothing known than
Middle Compeller Shale led below
Near Lawrence, drove entered L.
Black shale
5 1/2 ft Devt.
66 ft interval
spalling arg, silt)
shale,
modular arch
No Diastromageny
Lough exposed. 3 3/4 ft
thin bedded rock
fossils few
Argillite rock
with Cornwell brando
+ celticeras.
E. Near same time 3rd Wells, 1 mi
along road from North Fork up
North rising toward SE / 185?
6 ft Devonian L.
Spalling arg, silt,
33 ft (shaley layers,
modulus + Brachypora c.
18 1/2 ft arg exposures
Liptanana c. type of first section & thick
the entered L.