Image from the Biodiversity Heritage Library.
Contributed by Smithsonian Institution Archives.
| www.biodiversitylibrary.org
Transcription
173.
[illegible]
174.
The same rich frondiferous,
hnizens can be traced eastward,
almost to Hanington. At 174 only
the top of this horizon is seen, over
land by chalk hills.
175.
Lepidicera runs across here into
Fakel and.
Black shale
6ft. Devonian limestone.
7 1/2 ft not exposed.
4 ft light green soft clay,
modules.
6 ft Spalling clay.
3 1/2 ft softer clay stuff, fossils few.
Lepidocera, one but distorted.
3 1/2 ft frondiferous layers.
Top of Devonian L.
40 ft Devonian L.
22 ft not well exposed here. Probably
shale thin?
creek level.
176.
Adam. S impsons store.
Black shale.
3 1/2 ft Duffin Cages.
7 1/2 in Ber. limestone.
Section at Duffins end,
as the lower part of the Devonian
[illegible]
17 1/4 m, massive rock looks like
13ft bi.. Spalling clay arch,
6 in. Devonian crinums,
Lepidocera + Rhodocelata.
2 ft limestone.
19 1/4 ft Top of heavy l. layer with large
branching trygonos? not exposed
creek level.
177. Breey Devil, reaches creek level;
and retains type same as at 176.
178. Black Slate line reaches creek level.
Smith in road to Smith's whup,
road leaving a short distance
up creek path 174. Here the Black
Shale is by add 50 feet thick.
Limestone three full yrs modules
1-3 inches in length.
Conifers Gaporvady?
Road along creek leading S
into Smith's Fork, empties 2 mi E of Adam
Black shale
Devonian L.
20 1/2 ft interval
de next page.
2ft Platyenda. Volatropengia
Probably Umbilin but not Septata
found,
Interval not exposed.
D one colred l,
Shale bed.