"No exposures from here to the station called Barton. From here to the sharp curve h, the hillside are covered with much red-stained quartzite and pieces of the Clinton formation. The thickness could not be determined because there are no good exposures on the railroad runs near by or the line of strike. (There must be a fault from Barton joining up the Medina) (see Beothic lens) At the curve, where along Lockwood's Ferry, and mile post C. 393 is shown the following,