9) Residual blocks of developed Pendergra Come not definite, but Anheim, 974: argilla, clay, plat pendergra abundant. 51: after argill rocks plat pendergra, 52 ft cotten land. arg, cl, with plat pendergra. 106, A pressure anticline wrt. fracture at top, Mrs N 5 E. This pressure ridge crosses the Aurora east of the RR. 107. East of RR, Leptaena in lim part of Anheim, at track level, And cut up to Columnaria langer; measured clay & loose shell over fields It exposes NEY Rhenland. 108 15 ft 2 intervals to top of Hill. 2 ft residual with few Columnaria & by 64 ft Columnaria lager down to top of Anheim bed, as far as I could judge from experiences down creek. This drive must take into account the Southward dip, which in this distance is con siderable. The first place is 200 steps, Columnaria vocana Rock, when Columnaria's this field did not nearly extend toward top where it is harder. Southward the Columnaria's having drawn up first 3 hours. The mysterious Reifmann crump cos up on north endy, 109. From the creek up to grad corner grad road at 109, The base of the Platy, pendergra NW Anheim is 103 feet below the road crump. This = 950 - 103 = 847 The estimated number may be neara 860 while the measurements will trick along the road for at least 24 miles. 110 In town (Lancaster) is exposure of shale, about 5 feet thick, over with by from lifeless Anheim, below which is drive colored [illegible] Argheim base = 100. 111. Road level in say between two Lm's 360s sizes or "hills": Intervals 5-4 ft. basal part light blue fall J hugg, ans - layer of Riche mined. Upper part = shale, clay, by to Richmond. But in this is widely possible for us gone = Anheim with plat. pendergra are rather common and with me from Leptaena. Below this a drive colored lime stone. Below this is shale creek. The NW Anheim is not exposed here.