What is recorded here
Carn Naun Point is a headland in Cornwall composed primarily of Devonian slate, formed around 380 million years ago through deep-sea sedimentation and subsequent low-grade metamorphism. It is notable for its resistant rock formations that create a prominent coastal feature, typical of the Cornubian geological region.
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Places near here
Triangulation Point at the top of Trevega CliffCliff or headland · 216 yd
River CoveBay · 515 yd
The CarracksIslet · 1045 yd
Stone circle near Pen Enys PointAncient stone or rock art · 1180 yd
Standing stone near TrevalganAncient stone or rock art · 1233 yd
Rosewall Hill from TrendrineMountain or hill · 1641 yd
Trevalgan HillMountain / peak · 1.1 mi
Rosewall HillMountain / peak · 1.3 mi
Granite boulders on Trendrine HillMountain or hill · 1.5 mi
Towednack ChurchChurch, cross or graveyard · 1.6 mi
Hellesveor Methodist ChurchChurch, cross or graveyard · 1.7 mi
Porthzennor CoveBeach / strand · 1.8 miOther information
Photo: Robin Webster · CC BY-SA 2.0