Image from the Biodiversity Heritage Library.
Contributed by Smithsonian Institution Archives.
| www.biodiversitylibrary.org
Transcription
(24) Clinton fossils at Centre ville
Farms farm's.
Halynite Calymulatus
Stictoceras branchyng
Lyellia central bilateralis
Corthis, flabellites,
Trifidica Ctenum, complete very good
about 9 1/2 feet thin top of Clinton
Clinton at Bridge NE of town
is 20 ft thick. Bottom not seen.
Centre ville
Montgomery's mill.
Orelinmary section.
Waverly,
1 ft trainy, carb. shale.
4 in. varicolour layer.
6ft 3 in. Black shale.
6 to 8 in. Sandy.
28 ft limestone to base of black shale.
Colvert in road
57 ft to black shale base,
back.
15 ft. Clayey limestone, soft weathering.
72 ft. Total
solid limestone rest way up. 25
6 in. Shaly limestone.
9 in. Limestone
4 in. Shaly limestone.
1 ft 3 in limestone
3 ft limestone,
4 ft. uniform clay, fossils.
Nothing but rock from creek up to
this level. 43 feet above creek.
29 feet below Black shale.
Montgomery's Mill. Hickman Cr.
Completed section.
Waverly,
1 ft. trainy in carbonaceous shale.
4 in. varicolour layer.
6 ft. 3 in. Black shale.
6-8 in. Sandy layer,
shaly layers 4-6 in. thick occur
limestone, except at very rare when
25 ft to base of Black shale, also solid
Spinifer Andorea.
Phylinchymella Tennesseeus?
Platyctoma Virginicae.
Encalyptocorinus coelatus!
Encalyptocorinus fortius crassus
4 ft clayey fossils. Here Daffna records
above mouth of tunnel at mill
ville where he arrived. Total 43 feet
looks like the Laurel rock at Centre
28 ft. more solid limestone. Wyekee fault
not clearly distinct from rock above.
15 ft. Clayey limestone weathering back,
10 ft. From Duck river to base of section at
Montgomery's mill = rise of river.