Annual report . 1. Thirty chains southeast of bridge over Mississippi river at edge of small pon i. 2. Lot 24, concession II, Palmerston township, on old road. 3. East part lot 25, concession II, Palmerston township, at road side. 4. Lot 23, concession II, Palmerston township, north part of lot on old road. 5. Twenty chains east of Ompah post office at road side. 6. Two and a half miles east of Ompah, near talc prospect. GRANITE AND PEGMATITE INTRUSIVES These acid intrusives are the youngest rocks in the area, and have been found atseveral places, including the fol
Annual report . 1. Thirty chains southeast of bridge over Mississippi river at edge of small pon i. 2. Lot 24, concession II, Palmerston township, on old road. 3. East part lot 25, concession II, Palmerston township, at road side. 4. Lot 23, concession II, Palmerston township, north part of lot on old road. 5. Twenty chains east of Ompah post office at road side. 6. Two and a half miles east of Ompah, near talc prospect. GRANITE AND PEGMATITE INTRUSIVES These acid intrusives are the youngest rocks in the area, and have been found atseveral places, including the following: (1) At the northeast end of Madawaska (UpperTrout) lake a coarse-grained, massive granite, showing at times a well-developedgraphic texture, cuts the crystalline limestone, (2) A few hundred yards northeast ofOmpah post office a coarse-grained, granite-pegmatite cuts diagonally across the strikeof the gneiss and limestone. These granites and pegmatites may be of the same ageas the Moira granite at Eijf. 40. Hasting* conglomerate, showing squeezed pebblesPalmerston township, Erontenac county. 82 Bureau of Mines No. 4
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Keywords: ., bookcentury1800, bookdecade1890, booksubjectminesandmineralresou
