134 SUPERFICIAL GEOLOGY—HONEYMAN. 
This Archean (a) transportation seems to have been intercep- 
ted by the granitic band and superseded. The granites (g) are 
now transported toward the Atlantic. The (a) boulders have, 
however, evidently passed along the course of the Musquodoboit 
River and reached the shore, where I found them mixed with 
the granite (g) beulders. Glaciation was also observed at no great 
distance on an exposed surface of Lower Cambrian Argillites. 
In like manner at Clam Bay and Ship Harbour Lake whe 
there is also extensive glaciation, (a) are associated with (g). O 
the Bay we have apart of the Terminal moraine (a g) exposed to 
the storms of the Atlantic, where as at Cow Bay a “ Recent 
Formation ” is in progress. We shall again meet with these in 
the sequel. 
The “ Western Division” is in like manner sub-divided by a 
great range of granites (g.) extending from N. W. side of the 
“Central Division” along the South Mountain of Kings and 
Annapolis Counties. The Northern part of this Division consists 
of the south side of the valley that runs between the North and 
South Mountains, and the north side of South Mountain. The 
characteristic transportation is (t) from the triassie (T) rocks of 
Blomidon and North Mountain. I would here observe that the 
(a) of the Central (t a) and the Eastern Division does not put in an 
appearance in the West Division, although it crossed the Minas 
Basin it did not cross the Bay of Fundy from the Cobequid 
Mountains. 
We have examined this part at Wolfville, Kentville, Aylesford, 
and Nictaux. 
At the two last localities, glaciation was observed on thé north 
side of South Mountain, over which the (t) of North Mountain 
must have passed in its southerly course. I have not yet ex- 
amined the southern sub-division. Mr. Murphy, the Government 
Engineer, has traced the Nictaux glacial course along the Nictaux 
and Atlantic Railway. Vide paper in Trans., Vol. VI., page 150. 
In our Museum Boulder Collections, we have a boulder of gray 
Amyedaloid, which the late Peter Jack picked up at the Lunen- 
burg ovens. I have no doubt that the great granite masses which 
I observed in the fields on the road between Chester and Lunen- 
