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Contributed by Yale Peabody Museum of Natural History.
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Transcription
Monday Sep. 5 -1932
Wea. SAT. AUG. 21, 1909 Ther.
To define [illegible] cyl. locality is back of barn
the fair house north of Shells Corners. Beneath
it or near it is a thick zone of dol. in the Highgate but
the person with only Kniff and Laproce. Maybe 20
or 30 ft. thick, or 25'. Heck calls this dol. Milton = L.
Centra, and a thrust beneath resting on the high-
gate.
In the Highgate zone Laproce smaller than the others
of the large "Milton" dol 57' plus 8' of basal cong.
The difficulty in locating the thickness is due to the
arriving of the bed and a space eroded out.
At the road metal quarry 1/2 m. NW of Highgate
center Laproce agreed to the contact between the "Milton"
and the Parkin slate, but held that until prints are
frozen one can say that all is L.C. and mark the
contact as a local one.
Then Kilmer is the Parkin
slate followed by the dol. = the type of Parkins
crNile. There are to me several arguments this
makes his conclusion unacceptible. This cyl.
is clay made up of the dol. bedrock and the then redded
material associated with the dol. To me this cyl.
is the same as at the base of the dol in highgate
zone.