354 GEOLOGICAL GLEANINGS—HONEYMAN. 
actually passed along the hypothetical line of Mr. Fletcher's 
observation and reached Mabou Harbour accordingly. We then 
walked along the east side of the harbour at the foot of the Con- 
glomerates and drift observing our boulders as we proceeded 
embedded in the drift and lying on the shore, and reached the 
other boulders of preceding days, which had come directly from 
the Archzan rocks. We have thus found transportation from 
the mouth of the harbour to a distance below Mabou bridge—5 
miles direct. 
“Our GLACIAL PROBLEM.” 
The glaciation of Green Point suggests influences from beyond 
like the transportation on the Gulf shore in Antigonish County, 
and the glaciation on the verge of Cleveland Iron Moun- 
tain, Nictaux, and on the Canaan Road, Aylesford. The hypo- 
thetical parallels in Cape Breton and the natural sub-parallels of 
Lake Ainslie and Mabou Harbour conform with that of the Strait 
of Canso. We have already seen that the transportation and 
Harborus—Fjords—of Nova Scotia also conform with the Strait 
of Canso. The two thus conform with one another. Vide Nova 
Scotia on the Admiralty Chart and Fletcher’s admirable and 
thoroughly reliable map of Cape Breton. We have the latter 
mounted and on the wall before us which makes all this very 
clear. 
Locu Ban, 
We advanced still farther on Loch Ban than on a preceding 
occasion. As we proceeded on the east side towards Lake Ainslie, 
we observed Archzan boulders of the usual kind and variety on 
the road and on both sides of it. Special attention was given as 
we came near to Lake Ainslie. Here the Loch becomes a 
narrow neck. We now turn from the main road to the right and 
cross what seems to be a glacial moraine of considerable magni- 
tude. A deep hollow, a longitudinal excavation, causes a corres- 
ponding descent. Massive boulders are seen and examined. They 
are Syenites, Quartz-Syenites, and Diorites. Of these we collect 
specimens. We reach our terminus when we come to the lake. 
