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Proceedings of the Royal Society 
summit level of wliicli only about 200 feet above boulders. Through 
this gap boulders may have come ; but boulders are so cubical and 
sharp in angles that they must have been very gently lodged in 
present position. If they had fallen from any height they would 
have been fractured. These boulders have popular name of 
Claehan M‘‘hadf or “ Stones of the Fox ” {First Report, p. 45). 
(3) Above Pitnacree House, schist boulder resembling hypers- 
thene, 15xlljx4, differing from all rocks near it, called “ Clach 
Odharf or Dun StoneP 
Auchtergaven. — Granite boulder, 10 x 8 x 3 feet, weighing about 8 
tons, about 200 feet above sea, called “ DeiVs StaneP Longer 
axis N.E. Numerous cup markings on it. Supposed to have come 
from hills 30 miles to north. 
Aherfoyle. — Arndrum Hill is a ridge of the Conglomerate rocks 
which cross Scotland from Dumbarton by Callander in an E.N.E. 
direction. On this ridge near Aberfoyle (230 feet above sea) there 
are six boulders of greywacke, forming a line bearing N. and S. — 
each about 3 cubic yards in size, and from 2 to 20 feet apart from 
each other. To the west of this line of boulders, four other similar 
boulders lie along the ridge, stretching to nearly top of hill, viz., 
to 454 feet above sea {Ninth Report, p. 16). 
Blairgowrie. — Seven boulders of granite and mica schist, about 
200 feet above sea. No rocks of same kind nearer than Braemar 
range of hills, about 30 miles to N.W. 
Callander. — Gneiss boulder on top of Bochastle Hill, called ^^Sam- 
soFs Putting Stone,” resting on Conglomerate rocks. Longer axis 
N.E. In a very unstable position, being close to edge of a precipice, 
facing W.S.W., and about 330 feet above valley. About 50 feet 
below the above boulder there is another gneiss boulder, lying on a 
very steep slope of the same hill, facing westward, — from which 
quarter it must also have probably come {FBst Report, p. 46, and 
Second Report, p. 169) {Lithograph No. 37, Plate X.). 
Chinie. — Several boulders on tops of knolls. They probably 
have come from Grampians, which lie to N.W. {Second Report, 
p. 170). 
Crieff. — Two large Conglomerates, one called “ Witched Stone,” 
and two of granite, one called “ Cradle Stone,” lying on the 
‘‘ Knock ” Hill {First Report, p. 467). 
