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The bed of the river was formed by talc-schiste, in strata, the strike of which was from north by west to south by east, standing almost perpendicular, with a slight dip to the eastward. The stream was perpendicular on the line of striking. The pebbles in its bed were mostly basaltic, baked sandstone, conglomerate, quartz, sienite, and porphyry.
On them we found the only gravel bed we saw in Labrador, and yet their name is due to the rough piled basaltic appearing rock, that proved on close examination to be much weathered sienite and granite. The harbor is an open place amidst a cluster of rocky islets, and we found it literally packed with fishing vessels.
I did not ascend Mount McConnel, but it seemed to be composed of a species of domite. On the subordinate hills I observed sienite. The bed of the river furnished quite a collection of primitive rocks: there were pebbles of quartz, white, red, and grey; of granite; of sienite; of felspathic porphyry, hornblende, and quartz-porphyry; and of slate-rock. The morning was cloudless.
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