Jculamellona, Anostrophica are Syphidula galenta are seen. In other areas regular New York fossil New Zealand, (2) Below these limestones, to the east of the gravel down to the streams may be seen the shaly series of the New Zealand oolitic orbit: Cetylod reticularis; Rhipidomella Meta, Leptaena chesbricdoli. Also Peripha macrphylla, D. pulamellona, In about the middle of the thickness may be seen now a Camarcocinus payment. This zone is mostly of an 15 fut thick. Below these in the stream may be seen solid crinoidal limestones, the top layers of which have Camarcocinus in abundance and stems of what in New York would be called Mariacoccus (Smith nats). This is underlaid by the same limestone stone known on my former trip at Allens Mills - at the top of this series there is or here collected the species given in the N.J. A.M. How much of this solid limestone is Heldubuyian I can not say. The Camden effect is seen in many places along the roads, at nearly all the rivers enter the bottom lands. And now are three outcrops are meet the their zone of Camden clays formed upwards and by the iron bearing yellowish sands.