312 NOTES ON THE GEOLOGY OF BEDFORD, ETC.—HARE. 
River there was a great scarcity of them. All have red feldspar. 
Overlying the Archzean are great quantities of porphyritic granite 
boulders, rather darker than the Archzean granite in situ. 
The amygdaloids have been found westward as far as the 
School House lake, but not found farther. 
PLEISTOCENE. 
Striation.—The striation occurs in the gneissoid strata at Pock- 
wock lake. It runs north and south, and N. 35° E. It also 
oecurs in the gneissoid strata on the Margaret’s Bay road, running 
north and south and S. 10° W. I found it also on the argillites 
on the Hammond’s Plains and Sackville road, running 8. 20 E., 
also on the old Windsor road 8. 18 E.; also at Sandy lake, on the 
Hammond’s Plains road,and on the shore south of Bedford, north 
and south and south and north 10 east. The 8S. 20 E. iine pro- 
duced north-west passes Blomidon, and cuts a little to the east- 
ward of Cape Sharp, where trap rocks and amygdaloids are in 
situ (Partridge Island and Parrsboro’). The 8. 10° W. striation 
produced north-east meets the Wellington station 8. 25 W. stria- 
tion at the Gore. The latter striation produced northerly passes 
through the Londonderry iron deposits, and the archzean diorites, 
syenites, ete., of the Cobequids. 
