Field notes, Ohio, undated, 2 volumes
Page 31
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Transcription
quarry 3/4 mi N of Fairview School House Tmi E of Amity + 1/2 mi S wth. 2 ft cherty rock. 3 1/2 ft' Rather massive bedded luttles. 6+ ft Well bedded rock. resembling Springfield. As far as I can tell, the entire section, including the cherty rock at the top, may be Springfield. Some fragments cut coming from between like the Kitchenaria of the Red and the 1st & the Sphrodex relics rorwingeri) may come from immediately underlying Cedarville here At road corner 961, north of quarry, 4y mi. 6-thin bedded which doesn't seem to be the same as that at face of quarry last described. NW of Amity = quarry. 6 ft rock resembling Springfield at the lower quarry is more thinly bedded, which doesn't also resemble the Springfield Bearing 2 mi W of Drexel, 4 mi NW of Stop 5. More coarsely bedded L but no Cedarville fauna seen. - about 5 feet. 8 ft Well bedded L. Springfield with bent ammonites within 2 feet of base. Basal side of quarry, with arthur's labellites Pterocrinus gemmifrons stephencrinus scordium, & small crabs which may be? ?Heloplacoma ? ?3a? brachiopod signata? but the specimens are too poor to identify even approximately. East of Taylor crossing (Union City line) 1/2 mile, on road straight east to 6 mile house. N E of Brasfield = 915 US GS. Considerable Brasfield exposure here along side. Glacial striae S80E, Considerable exposure of Brasfield also east of C Road 936 going from the hill, cells below beneath. One mile E of Taylor crossing. W of 944 Brasfield topo = 922 US GS Glacial striae - S 80E about.