(43) 26½ ft not exposed. Partially sandy clay shale. 13 ft from gate top of clayey sand, exposed, IV fossils. 50 ft not exposed, partially sand clay shale, like specimens above? 1 ft dense limest. below 2 ft sandy shale with a few thin sth dense limest. bed layers 1½ dense blue limestone 5 ft I would like that called Gar dard 2 undet one... River. The dense limestones en- tain crinaceae, small gas trilobeds, large spines, all too possible to get out in excavation. Calam. section = 165½ ft. Calacaecia is erad. bed at top of well at level of dense formation 5 Colt Ferry, west if 9 ft fractured, clay and limestone Top; I want to close here, also some what near base typical. 6 ft very shifty, base not seen. 10½ ft clean forster calc. shale. 20 ft in lowest 3 layers. Base not seen. 14 ft Wst/nelida bed is fill of a large thin band of limestone. 2½ ft I understand the Whaffsela ella layer, before this new clayey west comes in topmost. 19½ ft beds thicker at base here. 5 in. White middle full for 34 parts, 3¾ ft irregular Clinton. 54 ft clay part of Richmond in the Lown well then traces of lime stone, apparently formed after depositing clay are formed in clay and recede some the clay in beds, a small limestone in certain parts. 9 ft from top of Whaffsela top clay l. Relative to strata at Calacaecia Streptoceras Streptoceras turn out small valves as parasitic. at base field in. Here also in turn is vertical valves? Strept. nevis retincta, 5 ft several specimens of streptolhoma at various levels.