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Updated: May 12, 2025
From an old tower, near this place, is an extensive view of Loch Braccadil, and, at a distance, of the isles of Barra and South Uist; and on the landside, the Cuillin, a prodigious range of mountains, capped with rocky pinnacles in a strange variety of shapes. They resemble the mountains near Corte in Corsica, of which there is a very good print.
Equally circumstantial is the same author's account of the relations of the granophyres to the gabbros, as seen at Meall Dearg and the western border of the Cuillin Hills where the former rock may be seen to send numerous veins into the latter.
These latter beds, throughout a considerable distance round the flanks of the Cuillin Hills, are interposed between the acid rocks and the plateau-basalts; but towards the north, on approaching Lough Sligahan, the acid rocks, consisting of granophyres, quartz-porphyries, and hornblendic-granitites, are in direct contact with the plateau-basalts; and, according to the very circumstantial account of Sir A. Geikie, are intrusive into them; not only sending veins into the basaltic sheets, but also producing a marked alteration in their structure where they approach the newer intrusive mass.
From an old tower, near this place, is an extensive view of Loch-Braccadil, and, at a distance, of the isles of Barra and South Uist; and on the land-side, the Cuillin, a prodigious range of mountains, capped with rocky pinnacles in a strange variety of shapes. They resemble the mountains near Corté in Corsica, of which there is a very good print.
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