Image from the Biodiversity Heritage Library.
Contributed by Smithsonian Institution Archives.
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Transcription
124
Aug. 3, 1908
At the head of the inlet near
the mill occurs a large mass of
gabbro over 100 yds. broad exposed
at and near the end of the mill on both
side of the pond and on the west
side of the inlet S of the mill.
This is flanked on the west by a
couple of feet of tough blue shales
striking N. 38° W. & underlain by
basal looking tuffs visible on the
north side of the mill pond in the
woods. The tuffs here strike N. 25°
W. Y dip 28° N.E.
The shale reappear under
the gabbro on the west side of the
inlet striking N. 25° W. & dipping
26° N.E. The tuffs beneath appear
on the point S. N.W. S. 1. 5. Drop
& gabbro form the shore down to the
road except for some dark looking
rhyolite tuffs caught up in the bed
near S.W. edge of S. 1. 5'. A thick
strike trends across the road N. 70° W.
dip along the shore, N. 70° W. brought down
of the new bridge appear some
and tuffs striking N. 12° W. & dipping
E. 25°
Bell's Mills
8. I.
4. 5