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Froceedings of the Boyal Society 
a still higher level on Ben-y-Gloe. Boulders of granite, gneiss, 
quartz, porphyry seen by Convener in the Bascally drift-beds 
{Second Report, p. 172). 
Killin. — On hill to west, about 1350 feet above Loch Tay, 
thick beds of gravel and sand; and therefore about 1650 feet above 
sea {Second Report, p. 173). 
On Morenish, east of Killin, and about 1100 feet above Loch 
Tay, several large boulders {Fourth Report, p. 31), of which sketch 
given. These, as shown by positions, have all come from westward. 
Kilspindie. — Seven granite boulders, from 5 to 6 tons weight. 
Five form a line, having a K.W. direction, all differing from the 
adjoining rocks {First Report, p. 47). 
Kirhmichael. — RocMng Stone, 7 x 5 x 2J feet, and several tall 
boulders near it, called Qlachan Sleuchdaidhf or Stones of 
Worship ” {First Report, p. 47). 
Logie Almond, — A whinstone boulder called Ker Stonef about 
48 tons in weight, on north bank of River Almond, near a bog ; 
“ Carr ” being Gaelic for “ Bog.” 
There is another boulder, a Conglomerate, resting on Old Red 
Sandstone, called “ Cid na Cloich,” or “ Stone Rook.” A stream 
forms a nook or angle with the drum or ridge, on which boulder 
stands. 
Another Conglomerate boulder on Risk Farm {First Report, p. 47). 
Glen Dochart. — The axis of valley is about E. and W. On its 
slopes facing the north, and near bottom, there are many large 
boulders of granite, which may have come from Ben Cruachan. 
They occur also on the ridges, on south side of valley ; — some so 
placed as to show transport from westward. 
At height of 1250 feet above sea, a vertical rock, well smoothed, 
with horizontal groovings on its west and north sides, indicative of 
some agent which has pressed severely on it in passing from west- 
ward {Fourth Report, p. 32) {Lithograph Ko. 38, Plate X.). 
Schehallion Mountain (top of, 3560 feet above sea). — Gravel beds 
indicative of aqueous action, seen by Convener, up to about 3000 
feet, to which height small blocks of a fine-grained grey granite 
seen. Side of hill with smoothest rock surfaces looks X.W. by W. 
Xo striae seen {Second Report, p. 173). 
Mr Jamieson of Ellon states {Quart. Journ. Lond. Geol. Soc. for 
