The Quebec rocks lithologically are not un- like the Loris and in this aspect alone we would regard them the same, Mr Adumaria occurs here and the gneissolite were said by Lapworth to be somewhat younger than the Normanskill. One also sees here enclavate gnos but all the pebbles are small compared with those in the Loris. We saw the valley all about the village of Silley and in the town it struck me that more plan shales occur than red ones. Driving along the river and the red hills are more dominant and as one go along the strata the oners seems. The very thick. As Loris is reported here but I could not feel thrilling that some is present here though the Loris lies, and enclavate are certainly absent here. We had Lunch at Kent Lodge, Mont- moranci Falls, Here again saw the Trenton- Archacan contact with masses of