refer are to about the Normansdill. From it in from the locality these Matthews identifies Tetrapodites. In the afternoon we went to the Fern Ledges. They are where the steps go down to the shore from the Park where the billy cars stop. These ledges are now not accessible. About one half mile further down the shore are large up bosses of sand, stones and openings I dark holes. All of these bits are hardened but are not ore- tamphores. In the holes occur plants. In one grow there was a great abundance of Cordaites leaves. These are large and long and at once suggest Pennsylvanic. All of the Germans are agreed that those measures are above the Culm.