Cornwall in focus

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The Geology of Cornwall

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Cornwall can really be imagined as a finger of 400 million year old Devonian slates along with Carboniferous sandstones and shales pointing across the Atlantic Ocean towards the USA, with a backbone of granite. The granite batholith forms moors at Bodmin Moor in the east and reappears in the granite outcrops near Roche in Mid Cornwall and in West Cornwall at the Carnmenellis Granite (dated at between 293 and 275 million years ago). The latter now largely covered by human habitation, south of Camborne-Redruth and in the far west at the striking and rugged landscape of the Penwith Granite. It is also present, but less apparent, due to its highly weathered or kaolinised state in the St. Austell Area where it appears as 'china clay'. Some excellent guidebooks are the heavyweight Geology of Cornwall by Selwood, Bristow and Durrance, Earth Story: The Shaping of Our World and the 'cheap as chips' West Cornwall: A Landscape for Leisure (Holiday Geology Guidebook) by A.J. Goode and M Leveridge Holder.

The Geology of Cornwall

Two very significant areas for both the amateur and keen geologist must surely be the tilted rock strata of the north cornish cliffs between Millook Haven and Woolacombe in Devon - see Earth movements and folding on a grand scale... The other has to be the metamorphic thrust zone of the Lizard Peninsula. An area of varied geology and landscape has essentially been formed by the collision of two tectonic plates. Examine a Map of the Lizard Peninsula or learn more about the complex Geology of the area.

Other areas to explore are:

Raised Beach at Porth Nanven, near St. Just
Contorted slaty strata at Godrevy Cove, near Hayle
Serpentine, Talc, Gneiss and Gabbro at Kennack Sands near Cadgwith
Steatite (or Soapstone) at Gew Graze (Soapy Cove), near Mullion
Marble Cliffs at Porthmissen, Trevone
Coloured Slates at Broadagogue Cove, Polzeath
Pillow lava at The Rumps and Port Quin
Volcanic ash and bombs at Trebarwith Strand
Goniatite fossils at Crackington Haven
Zig-zag (recumbent) folding in the cliffs at Millook Haven
Contorted and tilted sandstone strata at Maer Cliff, Crooklets Beach and Sandymouth Bay, Bude.

St. Michaels Mount  Lands End  Ancient Monuments  Echoes of an Industrial Past




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