are then cross to the or the Crule Trom an cliff, here the Bonarenture fills an old valley with the Mt Joli making the western slope of the stream, while on the eastern side is highly more Mt Joli (weathered) overlain near the Bonarenture contact by the Oriolay, or Pierce formation. The Oriolay in the bottom of the gorge and beneath the water fall stands at N 60 W and strikes N. 60 W, on the cliff B E. The Mt Joli on the west side has the same strike, but here the beds have slumped and are creeing down the hill. In the Mt Joli (weathered) should see no fossils at all. But the bedding surfaces are marked by "facies" that are identical in character with those of Mt. Joli. The vertical Oriolay yielded Leptoraelis and is some where seen in the unconformable Bona- venture. Continuity to Tof Mt at canoe Bmaranture In an cliff from a page slope of same valley Bonarenture Oriolay Mt Joli lies weathered red strike N.60 W weathered red The Oriolay again definitely observed. This contact was not definitely established on the Mt. Joli age because in the absence of fossils. On have we seen elsewhere the Mt. Joli weathered red. Storms ac- ccepted on the terms of wind Joli and full on Borel