Glaciation of Eastern Canada. 327 
Further to the east, at Lake Temiscouata and vicinity, 
Prof. L. W. Bailey and Mr. W. McInnes, of the Geological 
Survey, found striz and transported blocks, evidencing 
north-westerly ice movement from the summits of the 
water-shed." 
On the south-east slope of the mountain range mentioned, 
abundant evidence has been obtained in Canadian territory 
showing a general south-eastward ice-flow. Besides the 
striz met with in the Temiscouata Lake valley,’ I found 
others in the Madawaska River valley,’ also on the Quata- 
wamkedgewick, a branch of the Restigouche River.’ Striz 
have been seen also near the Matapedia Lake,’ and further 
east, near the mouth of the Restigouche, as well as in 
numerous places along the north side of the Baie des 
Chaleurs,’ all of which have a general south-easterly course. 
There were local deflections, however, caused by hills and 
river valleys, and especially by the slopes of the Baie des 
Chaleurs district. 
In the St. Lawrence Valley, on ledges below the 350 to 
375 contour line, strize and polishing were observed, indicat- 
ing ice movement in the general direction of the valley, 
that is, about north-east and south-west. These must have 
been caused by drift ice, as shown by Sir William Dawson ’ 
Co-ordinating all the phenomena relating to the glaciation 
of that portion of Quebec lying south of St. Lawrence 
River, we find that local glaciers upon the higher grounds 
and slopes and drift ice on the lower are sufficient to 
‘Science, Vol. VIII, p. 412. 
*Geology of Canada, 1863, pages 890-92. 
*Annual Report, Geol. Surv. of Can., 1885, Vol. 1, list of striae, 
part GG. 
‘Annual Report, 1886, Vol. II, List of Strize, part M. 
*Geology of Canada, 1863, pages 890-92. 
"Annual Report, Geol. Surv. of Can., 1886, Vol. II, list of stris, 
part M. 
‘Acadian Geology, 3rd ed. Notes on the Post Pliocene Geology 
of Canada, 1872, Canadian Naturalist. Transactions Royal Soe: 
of Can., 1886, Sec. lV, Art. X. Annual Report Geol. Surv. of Can., 
1886, Vol. II, part M. 
