Geological Society of America Bulletin

Cover Geological Society of America Bulletin
Geological Society of America Bulletin
Geological Society of America
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The pebbles are, however, of the same rock species as those on the shore of the lake.
This band of conglomerate is at least 16 miles long and 2 miles wide.
Its thickness can hardly be less than a mile and may be almost double that, since the dip is steep, but a covering of sand prevents very accurate measurements of the width. A very similar conglomerate appears on the east shore of Upper Manitou lake, 50 miles to the north, containing por- * Geol. Survey of Canada, 1H85, pp. 68, 124, and 150,
...CC.
t Ontario Bureau of Mines Heport, 1896, p. IrVj, etcetera.
Digitized by Google KEEWATIN AND COUCHICHING ROCKS, 227 phyry, felsite, quartzite, etcetera, and a fine example is found at Rat Por- tage, the matrix in this case, however, being sericitic instead of chloritic.
Numerous other instances are found in various parts of the region. No pebbles which are undoubtedly Laurentian have been reported from any of them, though granite boulders are found, as, for example, near Abrams rapids, north of lake Minnetakie.


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