What is recorded here
Cùl Cleite is a headland composed primarily of basaltic rock, formed during the Tertiary period through volcanic activity associated with the North Atlantic Igneous Province. Its notable columnar jointing and coastal erosion features make it a distinctive example of ancient volcanic terrain in the Outer Hebrides.
This does not grant access. Check current paths, opening conditions and ownership before entering.
Places near here
Southernmost point of Hirta islandIsland · 465 yd
RuabhalMountain / peak · 468 yd
GiasgeirIslet · 520 yd
Rubhal from the pier at Village Bay, St KildaHeritage place · 696 yd
Through cave on DunCave · 706 yd_on_Dun_-_geograph.org.uk_-_2253478.jpg?width=1280)
Bioda MòrMountain / peak · 719 yd
The Mistress StoneStanding or carved stone · 725 yd
Dun, with its natural archHeritage place · 1029 yd
St Kilda, Hirta, Clash Na BearnaichCleit (period Unassigned) · 1378 yd
Gob an DùinHeadland · 1381 yd
Bàgh a' BhaileBay · 1427 yd
Beach on HirtaBeach · 1.0 miOther information
Photo: Bob Jones · CC BY-SA 2.0