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Contributed by Yale Peabody Museum of Natural History.
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Transcription
-177-
Section 19 contd.
in diameter, may be traced laterally
10 yards into siltstone and sandstones;
matrix for these conglomerates mostly
quartz sand cobbles and pebbles both
chert and limestone but neither particu-
larly dominant; coll. 19-34 (15 feet
above base), Bryozoa fragments, Smaller
Foraminifera, Amphissites? sp.
Kegelites adjunctio (Cooper), Knightina?
sp., Bairdia spp. . . . . . . . . . . . . 160
33. Calcirudite, medium to dark gray weather-
ing, with matrix of fine calcite sand,
cobbles and pebbles dominantly lime-
stone, up to 5 inches in diameter, a
few small chert pebbles . . . . . . . . . . 8
Nealranch Formation
32. Shale, gray, some interbedded orange-
brown sandstones and thin conglomeratic
bands, largely covered, coll. 19-32B
(upper 3 feet), Pseudoschwagerina beedei,
Schwagerina emaciata, S. pugunculus,
Parafusulina? linearis?, Triticites
pinguis; coll. 19-32A (35 feet below top