Guide books of excursions in Canada1-10 . merly Robillard mountain) is a wellmarked topographical feature rising abruptly from Camp-bells marsh and extending as far west as the post roadbetween Combermere and Fort Stewart. It covers mostof the first four lots in Cons. XVIII and XIX, Raglan town-ship, the line between these two concessions running alongthe southern slope of the mountain. According to the meanof several observations with two aneroid barometers, it is595 feet (181-35 m-) above the marsh or 1426 feet (434-6m.) above mean sea level. The northern portion of the mountain is composedo
Guide books of excursions in Canada1-10 . merly Robillard mountain) is a wellmarked topographical feature rising abruptly from Camp-bells marsh and extending as far west as the post roadbetween Combermere and Fort Stewart. It covers mostof the first four lots in Cons. XVIII and XIX, Raglan town-ship, the line between these two concessions running alongthe southern slope of the mountain. According to the meanof several observations with two aneroid barometers, it is595 feet (181-35 m-) above the marsh or 1426 feet (434-6m.) above mean sea level. The northern portion of the mountain is composedof the reddish granite-gneiss of the Laurentian batholithso prevalent throughout the region. This gneiss is wellbanded as well as very distinctly foliated and containsthe usual amphibolite inclusions, for the most part elong-ated in the direction of the strike. This granite gneiss isintruded by many dykes and masses of granite pegmatite,often with a very marked augen, probably a proto-clastic structure, induced in the rock mass during the. Legend h±^_*d Gnt E~~j Gneissic granite I-* — *~| Gneissic granite cut by and nepheline syenites= —\ White, crystalline limestone ~-£[ Amphibollte s CraJpmont. Corundum Belt. MilesKilometres LOT 4. LOT S
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Keywords: ., bookcentury1900, bookdecade1910, booksubjectgeology, bookyear1913
