What is recorded here
Sròn Ghlas is shown as a headland on the public map of Highland. The saved point is the map point or the centre of its mapped shape.
Sròn Ghlas is a headland composed primarily of basaltic rock, formed during the Paleogene period through volcanic activity associated with the opening of the North Atlantic. Its columnar jointing and coastal erosion features make it a notable example of igneous landforms along the Scottish coast.
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Places near here
Tanera BeagIsland · 746 yd
Càrn SgoilteHeadland · 890 yd
Acairseid MhòrBay · 1062 yd
Creag na Coille DorchaMountain / peak · 1.4 mi
Sgeir DhubhIslet · 1.6 mi
Tanera More, Loch ArdHorizontal Mill (period Unassigned) · 1.6 mi
Meall MòrMountain / peak · 1.7 mi
Tanera MoreFindspot (20th Century), Bowl (steatite)(period Unassigned) · 2.1 mi
DornieBuilding(s) (post Medieval), Lazy Beds (post Medieval) · 2.6 mi
Old Dorney BayField Boundary (post Medieval), Lazy Beds (post Medieval), Slipway (post Medieval), Structure (period Unknown) · 2.9 mi
Priest IslandCave (period Unassigned) · 3.9 mi
The Summer IslesVisitor information · 4.2 mi