Field notes, Indiana and Kentucky, 1910
Page 103
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Transcription
Dam Steel's gap branch as far as Jackson, into the upper Farm munt is bylined but no drag walls fossils seen. At Trinity Huff the wulzing large shale bed comes down to creek level. About 1 mile eastward, the wulzing dwe crossed b. comes down to pipe level. Anti-cline at Rockyford 13 apt's at Church. 5 am mill 300 yds W., p. varying. at 2 am mill 4 1/2 mi W. Ranch and Ioni E by Rush Branch the dwe 1 D we crossed b. comes down to about 6 feet above creek. Rush Branch is 1mi W. y Marion-Carly Cr. line. 7 mi from Rush Branch to Bradfordville. Arr'd Tracy's at D.S.C.H. Batemans' home half a mile west of Bradfordville on the road to Merriamac. Chunnas's ranch. Section 12, mi W. by Rush Branch 5 to Merriamac. Platy dolomite. 15 1/2 ft. below Dev. limestone phosporus are dark colored bl. Do not know how far it has days dropped - along the road. Rapid Southward rise. Thickness unknown, owing to any exposure of shale bed, nodules irregular. 3 1/4 ft. fossiliferous l., a few agam. 3 ft. shale bed 3 1/4 ft. fossiliferous arg. siltstone limestone. 1 ft. Septaria b. 2 ft. dolomite crossed b. with Batemans' c.c.s. 3 1/2 ft. argillite, w/Shell fossils found.