Railroad bridge over Wilson Stream, - 1:50:4 (A) In the southwest corner where the rr. bridge crosses Wilson Stream, occurs in outcrop of some five feet of fine-grained, light-grey, dense sediment striking N.50 degrees west, dip- ing 72 degrees N.E. The rock resembles the Wilson Stream fossiliferous beds of "Hardscrabble", Dennysville. It is high- ly sheared. The shearing trends N.42 degrees east. A search for fossils revealed only an obscure impression of what may have been an Orthids (Delamerella), very doubtfully organic. The specia imen is 1:50:4 (A)