832 Proceedings of the Royal Society 
At height of 450 feet above loch, deep beds of a fine sandy clay 
occur. 
One of the boulders is at a height of 340 feet above loch, which 
corresponds with a horizontal terrace on south side of loch. 
18. Glen Morriston and Glendoe, on north side of Loch Ness , — 
(1) In Eighth Rejport (p. 15) Professor Heddle describes several 
boulders on the hills at the head of Glen Morriston, near Clunie 
Inn, at great heights, and some on very steep slopes, apparently 
transported from westward. 
(2) The Convener (^Fourth Report^ p. 23) describes a visit to 
Glendoe, at head of Glen Morriston, where he found several boulders 
of large size, at heights of from 919 feet to 1205 feet above the sea. 
These boulders rest on gravel and sand, and in height correspond 
occasionally with horizontal terraces occurring on opposite side of 
the valley where they occur. 
In a higher part of valley, viz., about 1190 feet above sea, deep 
beds of sand and gravel found. Terrace seen by Ordnance surveyors 
at height of 1280 feet, at top of glen. 
The Convener was told of a still larger boulder, about 1 6 feet high, 
at Clachnaharry, on south side of Loch Clunie, 2 or 3 miles west of 
Glendoe. 
19. (1) In Stratherrick, a large patch of grey granite rocks occurs. 
They are extensively quarried, and therefore are easily recognisable. 
Blocks have been carried eastward, even to near Elgin. They occur 
also on the tops of the Conglomerate hills between Loch Kecklis 
and Loch Hess, at heights of from 1400 to 1500 feet {Jolly ^ in Fifth 
Report, p. 72). 
(2) Along north bank of Loch Hess, near east end, a patch of red 
granite occurs, blocks of which have been recognised in the Tomna- 
hurich gravel hill near Inverness, and even on towards Hairn and 
Forres {Fifth Report, p. 69). 
Along south bank of Loch Hess, near east end, a peculiar liver- 
coloured Conglomerate rock occurs, blocks from which seem identical 
with a number of large boulders east of Inverness {Fifth Report, 
p. 71, and Sixth Report, p. 47). 
The late George Anderson of Inverness states that in some of the 
drift deposits near Inverness there are pebbles and boulders “ that 
appear to have come from very distant parts of the country. Such,” 
he says, “are the white stone of Ben Hevis and of Strathconon 
