352 GEOLOGICAL GLEANINGS—HONEYMAN, 
MABOU. 
We would now extend our investigation in the course sub-par- 
allel to the Highlands and towards Mabou. We begin at the Black 
River Road where our course was previously diverted towards 
Lake Ainslie, All the way we found Archean boulders: numer- 
ous when we approached the Archean mountains, less so when 
we were at a distance and had Lower Carboniferous hills inter- 
vening. Reaching Mabou River Bridge, we found them sufficiently 
abundant. We next proceeded on the road to the Harbour Mouth, 
and towards the 8S. West extremity of the Mabou Highlands— 
Archzean mountains. We found our boulders occurring all the way, 
and collected specimens. We next searched beginning at the 
bridge and proceeding up the river or away from the mountains, 
We walked as far as practicable along the E. side of the 
and found Archzean boulders all the way. We have thus ad- 
vanced in opposite directions in the hypothetical parallel line on 
the south-west of the Mabou Highlands. This conforms with 
glaciation observed by Mr. Fletcher at Green Point. 
Our next station is at the residence of Donald Macdonald, Ksq., 
the extreme S. E. point of the Mabou Highlands—Archzean. We 
have found Archzean boulders abundant enough up to this point, 
We now look around us. Archzan and Lower Carboniferous boul- 
ders are seen everywhere. We go to theshore of the harbour and 
find them equally abundant. Subsequently we ascended the only 
brook which proceeds from the mountain, and where a road to the 
pasture crosses the brook we found a good outcrop of rocks. 
We examine them and collect specimens. They are Archean, 
but so friable as to make it difficult to secure good solid speci- 
mens having characters which are exhibited by the transported 
boulders. This is the only outcrop which we can find in this 
quarter. We ascended the mountains. All is obscured by soil 
and luxuriant vegetation. 
GREEN POINT, 
We proceed to this Point. As we advance the mountains 
