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66.
Thus, at Labrador Pond, a line runs on both the west and the east sides.
In the valley running north from DeRuyter the two lines are as they should be; but the east line turns northeast along the upper part of the [[strikethrough]] l [[/strikethrough]] north branch of Tioughnioga; but the hill that runs parallel with DeRuyter Reservoir, is too low. It is wholly in Hamilton Shales.
So much I have today determined. The Stratigraphy is very simple; and it seems to me ^ [[insertion]] a [[/insertion]] little strange that Geologists have failed to discover what is so exceedingly plain.