What is recorded here
Cùl na Bèinge is a sea cliff or coastal rock feature composed of metamorphic rocks, likely of Precambrian to early Paleozoic age. These rocks were formed through high-pressure and high-temperature deformation of older sedimentary or igneous rocks, typical of the Scottish Caledonides, and the feature is notable for its association with the ancient geological history of the region.
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Places near here
Creag ÀrdHeadland · 175 yd
Doire na SròineMountain / peak · 683 yd
Tanera More, Loch ArdHorizontal Mill (period Unassigned) · 961 yd
Tanera MoreFindspot (20th Century), Bowl (steatite)(period Unassigned) · 1173 yd
PolbainCruck Framed Building (period Unassigned), Lazy Beds (period Unassigned), Stack Stand (period Unassigned), Township (19th Century) · 1349 yd
Old Dorney BayArchaeological Landscape (prehistoric) - (post Medieval) · 1404 yd
The AnchorageBay · 1609 yd
Creag na Coille DorchaMountain / peak · 1.1 mi
Sgeir DhubhIslet · 1.6 mi
Tanera BeagIsland · 1.7 mi
The Summer IslesVisitor information · 2.7 mi
Priest IslandCave (period Unassigned) · 5.9 miOther information
Photo: Chris Eilbeck · CC BY-SA 2.0