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At the same time, on the west side a stream was running north, and cutting a deeper and much narrower channel for the Onondaga River.
That this stream has always run northerly, since the great uplift, is manifest from the fall, now covered with drift, to the depth of 600 or more feet, looking north down that valley.
Water running north only could have cut Onondaga
River Valley.
Since the Tioughnioga heads here in several small streams, running south, it must have always run south, since the uplift. Here, therefore, has always been the water  divide, since it was first made dryland.