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[[image - pencil drawing of map showing landmarks and type of soil]]

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19 
the middle section, and some of the 3[[superscript]] d [[/superscript]] section, in the broken rocks below. 
The second exposure, 1/2 mile east northeast of Mr Dowd's house, on the east side of Tioughnioga, is considerably higher than the same rock directly opposite on the west side of the stream - not less than 25° higher, thus showing a decided flexure from east to west.
I could not get the Dip at any of these places -
Inequalities, in level, can be accounted for on no other supposition than inequalities of the ocean bed.