Field Notebook: Quebec 1924
Page 63
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Transcription
Then across the Townfield to sea cliff [100?] paces, all shale. Than about 30 paces more to low water of the sea, more shale. This originally belonged to, up [60?] ft. It's work bath along the beach I have a good view of Cornaunt rock and see that the strata stills caly the coast for [illegible] 1/2 mile. At the west end the strata are curturned to the S.W. about N° Farther off, in the Indian Point formation these rocks join for one verti- cial if a low dip measured the last time down here, it almost looks as if Cornaunt strata are about turning ~ the bottom of a syndine. 25 130 27 27 [17]5 91° 50 x 260 17,67 x 1.0 17,35.0 3.50