750 Proceedings of the Royal Society 
Campsie. —Rocks glaciated. Striations W.S.W. & W.N.W. (Re¬ 
porter—Ptev. Thomas Monro, D.D.) 
Fintray. —Boulders in a group, called “ Gowk Stones.” Have 
apparently come down valley. (Reporter—R. L. Jack (Geol. 
Survey).) 
Kilsyth. —Mica Slate boulder, 7 x 5 x 2J feet, about 6 tons. 1250 
feet above sea. Parent rock supposed to be 15 miles to north. 
(Reporter—R. L. Jack (Geol. Survey).) 
Ochils. —On watersheds of, at about 2000 feet, boulder of mica 
schist fall of garnets, apparently from Grampians to N.W. 
(Jamieson, “Geol. Soc. Jour.,” xxii. p. 166.) 
St Ninians. —Boulder about 200 tons, at height of 1250 feet above 
sea. (Reporter—R. L. Jack (Geol. Survey).) 
Strathblane. —Conglomerate boulder, 8x4x3 feet, about 7 tons. 
Longer axis W. 20° N. 1803 feet above sea. Parent rock 
supposed to be to N.W. (Reporter—R. L. Jack (Geol. 
Survey).) 
Sutherland. 
Assynt. —Two arge boulders, one at Unapool, the other at Stron- 
chrubie, called “ Clach na Putain ” (Stone of the Button). 
(Reporter—Angus M‘Ewen, parochial schoolmaster.) 
Clyne. —Remarkable kaims, apparently moraines (lateral and ter¬ 
minal) in valley of Brora. Also, rocks striated at Brora 
quarry. Striae run N.W. (Reporter—M. Myron.) 
Golspie. —Old Red Sandstone boulder, 16 x 10 x 4 feet, lying on 
Oolite rocks. Longer axis, N.N.W.; sub-angular. Sketch 
sent. About 248 feet above sea. Three smaller boulders of 
Old Red Sandstone lie about 100 yards to S.E. of the above. 
The Old Red Sandstone formation is situated to north and west, 
about 3 miles from boulder. Terminal and lateral moraines 
occur in Brora valley, broken up by diluvial action into ridges 
and hummocks. (Reporter—Rev. James Joass, minister of 
Golspie.) 
On the whole N.W. coast from Cape Wrath southwards, 
numerous “ Perched ” boulders occur on summits and sides of 
hills, in the most exposed positions. Especially numerous 
around Loch Maree. (Nicol “ Geol. Soc. Journal,” xiii. pp. 
29, 39.) 
