What is recorded here
Rubha Tolmach is a headland composed primarily of Devonian sandstone, formed around 400 million years ago through sedimentary deposition in a shallow marine environment. It is notable for its resistant rock formations that have withstood coastal erosion, contributing to the dramatic landscape of the Argyll and Bute coastline.
This does not grant access. Check current paths, opening conditions and ownership before entering.
Places near here
Oban, Kilbowie HouseCountry House (19th Century) · 274 yd
Unknown: Heather Island, Sound of KerreraAircraft (20th Century) · 490 yd
Gallanach RoadHouse Platform (period Unassigned), Quarry (period Unassigned) · 598 yd
Glenshellach RoadClearance Cairn(s) (period Unassigned) · 1009 yd
Ellery HillMountain / peak · 1046 yd
KerreraFindspot (20th Century), Barbed and Tanged Arrowhead (flint)(prehistoric) · 1069 yd
Bàrr DubhMountain / peak · 1284 yd
Port nan CuilcBay · 1482 yd
Viscount Kingarth: Oban Bay, Firth of LornSchooner (19th Century) · 1530 yd
The Horse ShoeBay · 1563 yd
Eilean nan UanIslet · 1.3 mi
Rubh a' ChruidhIslet · 1.4 miOther information
Photo: Patrick Mackie · CC BY-SA 2.0