782 
Proceedings of the Pioyal Society 
(3) Qhan.^Ki soutli end of town, there are cliffs of old conglome- 
rate roch, from which blocks have been carried southwards and 
are strewn on a meadow to a distance of from 100 to 200 yards from 
the cliffs {Semnhh Pejyovt^ p. 4). 
A plan given to show where these boulders situated, many being 
on hill slopes facing N. and INAV. These boulders are mostly all 
grey granite. 
On the hills, near Professor Blackie’s cottage, there are several 
large grey granite boulders on slopes facing N. and N.W. 
On small island in Oban Bay, several grey granite boulders, so 
situated, as to show transport from north [Seventh Reyort^ p. 7). 
On the farm of Dunbeg, near Connal Perry, a boulder of grey 
granite lying on rocks of clay-slate, in a position showing transport 
from iN’AY, [Seventh Report, p. 8). 
At Dunstaffnage, about 5 miles N.E. of Oban, the rocks smoothed 
in such a way as to. suggest movement over them of an agent 
from eastwo^rd, viz., down Boch Etive, Along the shore, up 
towards Loch Awe, there a^re rocks sinrilarly smoothed, as shown on 
the annexed woodcuts. 
WEST. 
EAST. 
Eocks smoothed from Eastward in Loch Etive. 
(4) At Lailt,” a dark porphyry boulder called Clach-a-CurraiV^ 
[i.e., perched houlder), from its precarious position. Differs from all 
the rocks in district. Eemains of a granite boulder also here. 
(5) Glenlonan. — Several boulders, at heights of from 1600 to 
1700 feet, of various kinds of rooks. Boulders are on both sides 
of summit level, but the greater number are on slopes facing the 
north, and the smoothed rocks also chiefly face the north. 
(6) Loch Etive. — At Airde Point, many boulders on slopes look- 
