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Contributed by Yale Peabody Museum of Natural History.
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Transcription
-149-
Section 8 contd.
Thickness
(feet)
siliceous replacement in upper 2 inches,
tetracorals common, coll. 8-25,
Schwagerina compacta, S. hessensis . . . . . 8
24. Limestone, light to medium gray weathering,
locally an organic fragmental rock, but
elsewhere a few feet along strike becomes
a calcirudite or chert conglomerate,
coll. 8-24, Schwagerina hawkensi, S.
tersa? S. diversiformis, S. compacta,
S. hessensis, Parafusulina schucherti . . . . 25
23. Covered . . . . . . . . . . . . . . . . . . . 5
22. Limestone, medium gray, organic fragmental,
locally over 30 percent limestone and
coll. 8-22
chert cobbles, 2 to 5 foot beds,
Leuox Hills Fm
18
21. Covered, probably brown-gray shale, . . . . . 26
Ross 1963
GSA
[C.C. MacC]
1996
20. Shale, brown-gray, Bryozoa fragments,
Smaller Foraminifera, siliceous sponge
spicules coll. 8-20
28
19. Calcarenite, yellow-brown weathering,
lower 8 inches have many pebbles, upper
4 inches are well sorted, evenly lamina-
ted, fine calcite and quartz sand, upper
surface is planar . . . . . . . . . . . . . 1
18. Shale, gray to gray-brown weathering, slightly
silty . . . . . . . . . . . . . . . . . . . 12