What is recorded here
Canglass Point is a coastal headland composed primarily of Carboniferous limestone, formed around 340 to 320 million years ago through the accumulation of marine sediments. It is notable for its exposure of layered sedimentary rock and its role in the geological framework of the Dingle Peninsula.
Places near here
SlievaghMountain / peak · 1040 yd
Enclosure in Kimego WestEnclosure · 1.0 mi
Man-made underground passage in Kimego WestMan-made underground passage · 1.2 mi
KilnKiln, corn-drying · 2.2 mi
Ballycarbery Castle (in ruins)Castle, hall-house · 3.0 mi
CastleCastle, unclassified · 3.0 mi
Foughil IslandIslet · 3.2 mi
White Strand BeachBeach / strand · 3.5 mi