of Edinburgh^ Session 1883 - 84 . 
801 
Cortacliy. — Wliinstone(?) boulder, 13x10x8. Longer axis E. 
and AY., supposed to have come from trap situated to N.W. 
Mica schist boulder within Earl of Airlie’s park. Parent rock 
supposed to be 2 or 3 miles to hT.W. {First Report^ p. 33). 
Far7iell . — Boulder weighing about 12 tons. Supposed to have 
come 30 miles from N.W. 
Inverarity . — Two grey granite boulders from 2 to 5 tons. 
Kirkden . — Kaims of gravel and sand 440 paces long, running 
E. and W. 
Kirriemuir . — Granite boulders, both red and grey. Supposed to 
have come from Aberdeenshire. 
Several kaims of granite pebbles and sand on Airlie estate, 
running KW. and S.E. {First Report, p. 33). 
Liff . — Several boulders of mica schist, called “ Gows of Gowrie.^^ 
A Druidical circle composed of boulders {Fwst Report, p. 34). 
Menmuir . — Two large granite boulders, each about 35 tons, 
besides others of smaller size. 
Montrose . — On Garnock and other hills, striae on rocks point W. 
by N. obliquely across hill. On Sunny side Hill, blocks of red shale 
derived from rocks in situ some miles to N.W. {First Boulder 
Report, p. 34). 
RescoMe.—FLmSb slate boulder 13x7 x 7, near top of Pitscandly 
Hill, lying on drift. Eocks in situ are Old Eed Sandstone. Late 
Sir Charles Lyall was of opinion it came from Creigh Hill, about 
17 miles W.H.W. Yalley of Strathmore lies between boulder and 
parent rock. There are also several hills higher than boulder be- 
tween it and parent rock {First Boidder Repo^d, p. 34). 
St Vigeans . — Gneiss boulder now destroyed. Supposed to have 
come from mountains situated to H.AY. If so, it must have crossed 
several ridges of hills and valleys. Kaim in the parish full of gneiss 
and granite boulders. 
* Haddingtonshire. 
Prestonpans . — A large basaltic boulder on the beach, known to 
the fishermen by the popular name of Johnny Moat,^^ in memory 
of a corpulent member of their class, who had formerly lived 
in the village. There being no basaltic rocks towards the east, the 
boulder must have come from the west {First Report, p. 18), 
