D. MILNE HOME ON THE PARALLEL ROADS OF LOCHABER. 597 
Thus the Lake which filled Glen Gluoy at its highest shelf, reached the 
summit level between that Glen and Glen Roy; and at that summit level an 
old River Channel was discovered by Ropert CHAMBERS and me, leading down 
to Glen Roy, at the timewhen Glen Roy was occupied by a lake, not only 
when this lake was at its highest level of 1149 feet above the sea, but alse 
when the Glen Roy Lake sank to the next level of 1068 feet above the sea.* 
So also at the summit level between Glen Roy and the Valley of the Spey, 
there is a flattish hollow, exactly corresponding in level with the highest shelf 
in Glen Roy, over which the Lake in Glen Roy when at its height of 1149 feet 
above the sea could discharge its surplus waters. 
* As this is a point of some importance, it is only fair to state, that a very experienced observer, 
Professor Nico of Aberdeen, does not admit that there is evidence of a River Channel from any one 
Glen into another Glen. He says (“ London Geol. Socy. Journal,” May 12, 1869, page 284) “I examined 
the various passes carefully, and found that whilst in none of them was there the slightest trace of an 
ancient river, in all there were distinct indications of the former existence of a narrow Sea Strait.” 
The valley by which the Gluoy Lake is assumed to have drained into Glen Roy is very narrow, and 
encumbered with detritus from the hills on the sides. The summit level is flat and marshy, and it 
appeared to me considerably below the level of the line (é.c., the ‘Road’?). On the other hand, a line 
of stones, as if washed out of the detritus, appeared to show that the sea or loch, had extended quite 
through the Strait. I observed no indication of any stream of water, larger than the present small 
rivulet, having ever been there.” 
In answer to these statements, I give the following Extracts from the Notes made by me on the 
occasion of my visit to the place with Robert CuamBers, in September 1846. 
“ At the head of Glen Gluoy, Shelf 1 almost disappears in the Moss. It is however faintly visible 
on the North side, about 1 or 2 feet above the Moss, running towards Glen Turrit. The Moss I found 
to be 54 feet thick above Boulder Clay. About 14 miles to Eastward, found rocks in middle of 
Channel, much worn and smoothed,—their rough edges or faces all pointing Eastward, 7.e., towards Glen 
Roy. This is near Glen Turrit, and about the place where traces of Shelf 1 disappear. About 8 or 
10 feet above these smoothed rocks there are other rocks which present no appearance of smoothing. 
“ At the side, there are low grassy knolls or hummocks apparently marking edge of a River Course,— 
which here 40 yards wide. 
“Apparently Gluoy Lake continued to discharge, whilst Roy dropped from Shelf 2 to 3, hence 
additional cutting power given to Gluoy Stream ;—and accordingly there is a deep and rocky ravine, 
down to Glen Turret. 
“Measured with Ropert CuamBers (who first drew my attention to fact) depression of Shelf 2 in 
Glen Roy below Shelf 1, and found that by Spirit-levelling, it was 29 feet ; by Sympysometer 35 feet ; 
by Barometer 11 feet. 
“Visited next, head of Glen Roy, in upper Glen Roy. Interesting to observe how uniformly the 
smooth surfaces of rocks are to West, the rough faces to East.” (Notes p. 47). 
The following applies to the Glen Glaster old River course. 
“ Discovered debouche of Lake No. 3 in Glen Glaster. A Shelf on both sides runs up to Col, at a 
level coincident with Moor there. 
“ At this place, rocks appear above moss. These are about middle and lowest part of flat—Evi- 
dently, water has rushed over these rocks from West: for their round and smooth faces are to West, 
their rough faces to East. They form a Channel sloping down towards Loch Laggan for about a mile. 
By existing burn, they can’t have been rounded, as this burn, very small, and 20 feet below them. 
These rocks occupy a breadth of from 30 to 40 feet, and have evidently occupied bed of a stream, 
exceeding that width. Walked along this supposed ancient water-course for about a mile, and saw that 
it extended down towards Loch Laggan, as far as eye could reach, Probably Loch Laggan then stood 
at level of Shelf 4, discharging itself at Mukkoul, as it continued to do, when Lake Roy sunk to 
Shelf 4. 
“ No sand or gravel in this old Water-course, but numerous granite boulders, very spherical. 
“Remnants of sloping haughs on each side, evidently formed by old River when in flood,—with 
precipitous cliffs beyond these haughs,—indicating height to which floods reached.” 
