Mr M'Laren, in his “Geology of Fife and the Lothians,” states:—

“There are few opportunities of observing ‘groovings’ on the Pentland Hills. I noticed them, however, at Westwater of Dunsyre, on the top of a thick bed of hard sandstone, from which 12 or 14 feet of alluvium had been removed. The dressings pointed exactly east and west; and the evidence was the more satisfactory, as the direction of the stream on whose bank the rock was situated, and of the valley in which the stream flowed, was south and north. They were very distinct, the larger groovings being about 1½ inch broad, and ths of an inch deep.