What is recorded here
Àird Beag 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 resistant columnar jointing and coastal erosion features, typical of the Scottish Northwest Highlands.
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Places near here
Loch KernsaryBuilding (period Unassigned), Crannog (period Unassigned) · 659 yd
KernsaryBroch (iron Age)(possible) · 978 yd
Loch MareeGeneral View (period Unassigned) · 1.5 mi
Allt A' Pholl-choire, Clapper BridgeRoad Bridge (period Unassigned) · 1.6 mi
Creag Mhòr ThollaidhMountain / peak · 1.8 mi
Alexander Cameron, the Tournaig Bard Memorial CairnMemorial · 1.9 mi
Inverewe GardenHeritage attraction · 2.1 mi
Camas GlasHeadland · 2.3 mi
Camas a' Bhaid LeathainBay · 3.0 mi
Meall an SpardainMountain / peak · 3.0 mi
Eilean a' Gharbh UilltWood · 3.9 mi
Eilean Ruairidh MòrIsland · 4.1 mi