Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
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Transcription
Thursday August 25 -1932
Wea. Mon. July 12, 1909 Ther.
above drifts late
The Beapla slate between in grey slate
without is pieces.
Above 5' high a
few piecs of the lentic to are introduced, and 10' above
base they are more common and the piece length up to
10". Then for 10 once they are no more common,
and the quarrying is to regularity. Dracantim is cold.
give thin rows in thickness up to 4" to 8" thick. There
is only thickness of cyl. Towards the road about 300' to
E.
to the N. the E-W. road
Above Middle Cambrian place to Duff Rim outcrop
guns across
farthest S, is 75 yards long. Then a head of 70' to thend
by another outcrop of 20 yards. The cyl. have thickness
of 6-7" with blocks of 108' long. Location is the Wen
to St. Albans slate, and where the joints come from.
arm to slates
--> Dr. 360 perhaps the first zone of dol. a zone 10'-20 thick
and dipping to E.10°. As those dol. are unknown in the St. Albans,
this zone must be in the upper Parthen. There may be more
Parthen on the left if it has the same. The determined units
from are collected. From this dol. to the Dr. to the Duff Rim
is cyl at a 360' across. In certain once along of this dolo'd
seem is decidedly any metamatized and is thus in the Ruff
Brith cyl. made up of dol out of the uppermost Parthen
slate. We can have the actual thickness here also of the
St. Albans.