Excursion in Eastern Quebec And the Maritime Provinces Excursion A1 volume 2
Excursion in Eastern Quebec And the Maritime Provinces Excursion A1 volume 2
Geological Survey of Canada
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Flinty slate and grit with intru- sives of granite, rhyolite, dia- base, basalt, and monzonite. O + 00 + o o + o 0) + o o ID + o 00 I/O s s SI 01 3 r»-. 3 2 'u "> o Ih o . 2 "o ■> c 3 . 2 'C _3 t/3 35063— 6|a 292 Antigonish to McAra's brook. The town of Antigonish (alt. 40 ft. , 12 m. ) is situated in the valley of Right river which follows what is apparently an ancient depression, now partially filled with the Car- boniferous rocks of the McAra's Brook and Ardness for- mations, the latter of ...which immediately underlies the town. Less than a mile to the north of Antigonish the surface rises rapidly to the plateau, here underlain by the James River rocks, through which protrudes a core of diabase forming the elevation known as Sugar Loaf hill (alt. 760 ft. , 213 m. ). This portion of the plateau is separated from the larger area to the west by a lowland whose surface rocks belong to the McAra's Brook forma- tion and through this lowland the Gulf road follows the valleys of Right river and Malignant brook to Malignant cove.
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