Field Notebook: Quebec 1924
Page 58
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Transcription
Just E. of the Barite, there is a road to the N. and over by the Barite river. Marked N. The reason why the Lignite lies so near farther is because the land is low and all is mowed into lower or older strata. Bring up the Kings Road See me shaly rock that may not be in place. It's in it dips 80° S. & strikes N. 75° E. This is just at the end of Barite, Farther N. on Kings road See a rock nearly horizontal. Dip slightly No. It may not be in place. On King farther W. marked me and the dip is 30° S.W. Strike N. 130 E. There now and there and seems to dip into the Barite Camp. It rolls like Tournum, having due the trails. The hills are all high to the N.W. Then left the Kings Road and to the south of it saw a thin outcrop of Red Lignite Eridophyllum. It may be the same zone seen along the railway. The mining. The private road down on