North Cornwall is an area of outstanding natural beauty that is of great geological and scientific interest. It includes the only part of Cornwall that is formed ofcarboniferous rocks, the northern area of North Cornwall District. The rest of the district lies on Devonian sedimentary strata and the granite of Bodmin Moor. A similar area is covered by theNorth Cornwall parliamentary constituency.
North Cornwall has a stretch of coastline that borders theCeltic Sea to the north. TheCarboniferoussandstone cliffs that surroundBude (and stretch down as far south asCrackington Haven) were formed during the Carboniferous period, around 300 million years ago. They are part of what are known to geologists as theCulm Measures which continue eastwards across north Devon. The folded and contorted stratification of shale and sandstone is unique in southern England. During theVariscan Orogeny, which affected the entire Cornish coast, the cliffs were pushed up from underneath the sea, creating the overlapping strata. As the sands and cliffs around Bude contain calcium carbonate (a natural fertiliser), farmers used to take sand from the beach, for spreading on their fields. The cliffs around Bude are the only ones in Cornwall that are made of Carboniferous sandstone, as most of the Cornish coast is geologically formed ofDevonianslate,granite andPrecambrianmetamorphic rocks). The stratified cliffs of Bude gave their name to a geological event called the Bude Formation.[4] Many formations can be viewed from theSouth West Coast Path which passes through the town.
The larger harbours are at Padstow and Bude and on the intervening coast Port Isaac, Port Gaverne, Port Quin, Port William, Tintagel, Bossiney and Boscastle have all been used either forfishing or the export of slate. There are good beaches at Polzeath, Trebarwith Strand and Bude. At Delabole the large Delabole Quarry has been worked for many centuries and there were once in the parish of Tintagel many other slate quarries. Granite andelvan have also been important minerals: there are major granite quarries in the parish of St Breward and also some china clay works on the edges of Bodmin Moor e.g. at Stannon nearCamelford.
Most of the lowland areas have good agricultural land used either for mixed or dairy farming. At Davidstow much of the milk is processed intoDavidstow cheese.
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