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Contributed by Smithsonian Institution Archives.
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Transcription
5°9" Crossbedded chinkm, at present
very f[illegible] in places.
5°9" greenish Ordovician clay ac.
finally exposed.
clim up with
favarites favorn? flat with
corallides 3 mm. across,
Habyrite catenulatus
dicranus ambiguus type, (Legrand?)
3D. Ordovician W.M Harward's on road
to Trace creek, N of Buffalo river.
14½" Clay
8° weathered clay limestone - Mr pressic
at least some 6 mm.
11° Fossiliferous weathered clay rock.
Fossils chiefly in upper half.
32 Mt. Ed. Walker - on Tucker Branch
road.
50¾" Sandstone, greenish = Warally
8" to much finegrained rock full of
discophute nodules up to 7" thick,
1° Black shale
4" Sandstone.
1° 8" Dark shaly fine grained ark
with Lingula subsquata. Takes the
place of the phleplate rock at base
of section at Pegrambridge.
Further down the road at a spring & farther
Sandstone = Warally + phleophate nodules.
Black Shale
1° 8" Shaly rock.
7° Fine grained sandy rock. This
can hardly be Silurian. It does
not show evidences of layering.
3° 8" clay.
10° 8" clay rock spalling.
B 5° 9" Calcareous clay Fossils.
5° 6" limestone, upper part is a shaly lime
stone.
3° covered
3° limestone.
B = Favarites Forbesi, Dicranus Clifton
pentagonus type. The Roemer bygogram, lim
spider's disc abraded.