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Transcription
11
2 ft. chiefly clay, rest well exposed.
10 in. thin limestone,
10 in. chiefly clay,
9 in. massive limestone,
6 in. clay,
5 in. massive limestone
2 ft 5 in. chiefly clay;
2 in. thin clazy limestone full of large crinoid heads
2 in. clay.
4 in. limestone, partly white needles a short distance further west - 20 ft to bridge.
= 19 ft of Chint according to these measurements.
The local Oxford layers from their source material in this district are always shaly and planar + Stri telazema.
82 ft. between base of Clinter & base of Conifers west f Slate Cuth.
Crnp. at top 4 ft 3in. 1/4 in. like brecciated rock but without breccia
1½ ft. brecciated rock below,
1½ ft. fully chert, almost all chert at least 5 feet of rock with chert + with clazy chalk.
82
20 4
61 8
15
20) Enroad leading to Heward's Mill
½ mi. W of Spencer,
Blue clay rock, Ordovician. Good section f about 40 feet. Claygy matrix.
3 ft. local massive Richmond Shry.
telazema. Within bipinata large large crinoid stems.
2ft 6 in. thickest nos layers 2 in thick with clay partings about 4 in. thick.
11 in. lower half of same. Upper clay clay rich with byzovana to, per
5 ft. 6 in. chiefly clay with a few thin limestone layers 1 in. thick.
The limestone is a very small part f this section.
6 inches several thin node layers with Rhynchotella cafaux.
Cortus or indeters & subgrydae
Orthis bipinata lower S.2.
Simple mena
Rafineszonia
simple mena, jplanumbrana
small from wt 5 mil
Ordred ventral area +
strong brian along an
turn + lateral edge.
1½ ft. limest. Rafineszonia. Very good Strph! planumbrana
28 ft clay at top limestone with Rafineszonia, Simple sulcata
20 ft to base of Clint m. clay.