also take specimens. Advancing to the summit we find similar 
boulders as far up as the top. We have reached an elevation 
which commands an extensive view. We see the Highlands over 
the Strathlorne sand hills, which we now regard as a glacial Mo- 
raine. We take levels and find that we are on a height correspond- 
ing with Fletcher’s Archzan border and junction of the Lower 
Carboniferous Metamorphic. We descend the mountain in the 
homeward direction and find a considerable outcrop of a coarse 
conglomerate. Reaching our headquarters we examined Fletcher's 
map to locate our outcrops and found an observation 75° dip, 
We are not aware that he noted the occurrence of the Archean 
boulders as we have not with us any of his Reports. We consider 
their occurrence at this elevation very important in its bearing 
on the height of our glacier, and its relation to the 1000 feet 
summit of Cape Mabou and associate elevations. 
Proceeding on the road toward Mabou and in a course sub- 
parallel with the Highlands, with the strath and river on our 
right and the sandy Moraine on our left, we observe Archean 
boulders in great abundance. The sand hills are succeeded by a 
mountain, on whose sides the rocks outcrop so as to be distinctly 
seen from the road. We cross the bridge over the river which 
here proceeds direct from the mountain gorge under the name 
of McAuley’s Brook. Tracing its course on the map we find it 
coming from the one side of Cape Mabou, while other brooks 
proceed from the Cape in an opposite direction, toward the Gulf. 
We continue our progress along the road, still observing abund- 
ance of Archean boulders. Coming to a road ascending the hill 
on the left, we turn in this direction. Archzan boulders are ob- 
served up to the top. Continuing we descend on the opposite 
side, still observing Archzan boulders on our way, some of them 
of large size. We collect specimens. Advancing we come in 
sight of Loch Ban and Lake Ainslie. We have now on our right 
a deep hollow witha brook (?). We follow this until we reach the 
low ground and swamp, which reach to Loch Ban. We have now 
the mountain with the outcropping Carboniferous rock very 
loftily in the rear.. Away on ‘the right Black River with its 
dease woods is seen, also proceeding toward Lake’ Ainslie. Our 
350 GEOLOGICAL GLEANINGS—HONEYMAN. 
