"If this can be worked out easily by using Van Ingen and Clark's table in the District Fm. Rocks in the vicinity of Randwy, N.Y. Left Kingston at 4.35 for Port Jervis a railway mt connecting with the others at Randwy. Got to P.J. at 8.05 Staying at Bours Hotel. The contact between the Cliff Hill and the Hudson River is striking and angularly un- as Randwy correlative. The two surfaces are of grey different materials and from though the H.R. is largely a sandstone yet there is no sand in the Cliff Hills. The surface was clean when the sea came and had been eroded quite flat. See sketches or penins fogs For contacts see my old photos.