Field Notebook: Nova Scotia, Quebec, Vermont 1924, 1928, 1932, 1933
Page 197
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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.