of Edinburgh, Session 1879 - 80 . 605 
besides many other conglomerate boulders — as at the following 
places : — 
On Landrick Estate, one weighing about 360 tons (p. 43). 
At Keltie Bridge (a mile east of Callander), one weighing about 
60 tons (p. 45). 
On Gartincaber estate, one weighing about 16 tons (p. 43). 
On north side of Teith, below Landrick Castle, one weighing about 
13 tons (p. 44). 
In the Burn of Cambus, two weighing about 13 and 24 tons 
respectively (p. 44). 
In the district traversed by the hill road between Doune and 
Callander, there are multitudes of conglomerate boulders of smaller 
size (p. 44). 
At Cornton brick- work (between Stirling and the Bridge of 
Allan) I saw a small conglomerate boulder found in the clay-bed 
there. 
On the rocks adjoining Stirling Castle on the north, I observed 
small conglomerate boidders , besides some of gneiss and greywacke 
(p. 39). At Loch Coulter and Gillies Hill, places about 3 miles 
south from Stirling, and from 400 to 600 feet above the sea, I 
found several conglomerate boulders , besides some of mica slate and 
felspar porphyry, evidently all brought from the N.W. 
On Plean estate (4 miles S.E. of Stirling), besides boulders of 
granite, gneiss, greywacke, and whinstone, there were some of con- 
glomerate (p. 46). 
At Glenbernie, near Torwood (5 miles S.S.E. of Stirling), I found 
a conglomerate boulder about 6 feet square (p. 48). 
On Dunmore estate (about 9 miles S.E. of Stirling) there is the 
Carlin Stone, a conglomerate boulder weighing about 10 tons. 
This list of conglomerate boulders may be considered interesting, 
as the position of the parent rock is known, viz., the band which 
traverses the country at Callendar, running from that point N.E. 
towards Brack] and, and S.W. towards Aberfoyle and Loch 
Lomond. 
Assuming that the boulders have all come from this band of con- 
glomerate rock, they show a transport from the H.W. They also 
show that they cover a wide district of country towards the S.E., not 
a district forming a valley, in which a glacier might have moved, 
