Field Notebook: New Brunswick, Nova Scotia, Quebec 1905
Page 109
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Transcription
here there is more limestones. Baspe gone 2 above the fault begins with the same kind of beds as those of gone 1. In fact they are the same beds continued on these gon gradually into a soft shale series bluish- green with purple goes. These shales are of gone 3, a soft series easily weathered away, but of considerable thickness. Not a trace of fossil in them. Gone 4 is again a limestone reminding of a rotulime stone as at Buffalo N.Y. The only prints are crawling worm trunks and a small Conularia which fails to get. Also like this: [sketch of triangle]