means another well between the Lorrville and Amsterdam (only = Blyed River). Here also occurs a little of the Black River for Chumnaria alveolata was found. The Lorrville is here full of passages, typical and of very large orge, up to half inch in dia- meter. In the afternoon autored to Cushing Realit (see hi Herlimer Co. N.York) along King Creek and Middletown. At the bottom of the Creek may be seen the Beelmantown, disconformity On it rests, the Lorrville, 15 feet thick, in a series of un- dulatory beds, the undulations due to the uneven surface of the Beellmantown. Almost throughout the minute bridges are more marked some of them encroaching and some intra form expl. Common but none of the large ones. Near the middle there is a There is no Amsterdam here on any Black River. The Trenton rests disconformally upon the Lorrville which is a close light blue and heavy bidded limestone almost devoid of fossils, while the Trenton is dark blue, thin bedded with these lasting and abundantly fossil- forms. They may not be actual Lower Trenton. In the basal beds de. testudinaria and P. seri cens are as evidently common, Le. so are Electrotta.