836 
Proceedings of the Boyal Society 
On several parts of the hill, especially on its south slopes, the 
rocks are broken up into large cubical fragments, resembling, in 
shape and composition, the boulders mentioned in (5) above {Second 
Report^ p. 163). 
(12) In the Ninth Report (pp. 10-12) there is an interesting 
list of boulders in the neighbourhood of Inverness by Mr Wallace, 
High School, Inverness. 
(13) Kingussie. — On Clunie M‘Pherson’s lands, two boulders of 
a coarse-grained granite. One is 1 1 x 9 x 6 feet, the other is about 
double the size of the former, with felspar crystals of a green colour, 
and mica plates about 1 inch square.* Longer axis of both, about E, 
and W. Both lie on a hill-slope, facing down west. Height above 
sea 1035 and 1080 feet. Eocks of district are clay slate. 
The nearest hill is Craig Dim, situated 4 miles to north on 
opposite side of Spey, the rock of which is also clay slate. 
Another boulder on Belville estate, 2 miles from Hewtonmoor 
Eailway Station, from 950 to 1000 feet above sea. Greatest length 
14 feet, breadth at top 8 feet, height 9 feet. Longer axis S.S.W. 
At Laggan Free Church, a well-rounded granite boulder, 9x6x6 
feet, with longer axis E. and W., corresponding with directions of 
numerous strise on a well-smoothed rock on which boulder lies. 
Nearest hills of granite are some miles to the west. 
KlNCARDINESHmE. 
1. Banehory-Devenieh, near Glassel Eailway Station. Boulder 
called ‘‘ Bishop’s Stone”; circumference 44 feet, height above ground 
8 feet, estimated weight 70 tons. Bluish granite, differing from 
adjoining granite rocks. An ancient stone circle of boulders about 
200 yards distant. 
About 2 miles to north, rocks on Hill of Farre glaciated with 
strise, running E. and W., — parallel with axis of Dee valley. 
Fettereairn. — No boulders now in parish, of any size. Long banks 
of sand and gravel, running parallel with one another. 
2. Maryeidter. — Boulder 5J x 6 x 6 feet. Longer axis N. and S. 
Eock of boulder supposed to be same as rocks to eastward {First 
Rep>ort^ p. 40). 
* The only other boulder with felspar and mica crystals, similar to those met 
with by Convener, is that mentioned as occurring on Treshlik Hill, p. 63. 
