What is recorded here
Àird Caol is a headland composed primarily of basaltic rock, formed during the Paleogene period through volcanic activity associated with the North Atlantic Igneous Province. It is notable for its role in the dramatic coastal landscape of the Western Isles, shaped by erosion and tectonic processes over millions of years.
This does not grant access. Check current paths, opening conditions and ownership before entering.
Places near here
Rubha GlasHeadland · 265 yd
The beach at RhenigidaleBeach · 523 yd
New house, ReinigeadalOld home or work place · 535 yd
Harris, RhenigidaleHead Dyke (post Medieval), Township (period Unassigned) · 613 yd
Mountain terrain above Loch SeaforthMountain or hill · 1145 yd
Loch TrolamaraigBay · 1365 yd
The beach at MolinginishBeach · 1645 yd
Harris, Abhainn A' GhlinneCairn (period Unassigned)(possible), Shieling Hut(s) (post Medieval) · 1.4 mi
TòdunMountain / peak · 1.7 mi
Todrun MountainMountain or hill · 1.7 mi
Leac EasgadailMountain / peak · 1.8 mi
Cairn at the head of the pass over to Loch TrollamarigAncient tomb or cairn · 2.0 mi