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Variscan coast: Difference between revisions

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The Variscan orogeny was a mountain-building event that gave rise to Cornwall, along with other mountain features across Europe. This was caused when the ancient continents of Euramerica and Gondwana collided to from the supercontinent of Pangaea. The granite that rose towards the surface under what is now Cornwall distilled many elements from deep in the earth into the existing ('country') rock, as it partially melted in the margins around the granite.  
The Variscan orogeny was a mountain-building event that gave rise to Cornwall, along with other mountain features across Europe. This was caused when the ancient continents of Euramerica and Gondwana collided to from the supercontinent of Pangaea. The granite that rose towards the surface under what is now Cornwall distilled many elements from deep in the earth into the existing 'country' rock (known in Cornwall as 'killas'), as it partially melted in the margins around the granite.  


It was these areas that would very much later be mined for their wealth.
It was these areas that would very much later be mined for their wealth.


For more info, see this amazing website: [https://variscancoast.co.uk]
For more info, see this amazing website: [https://variscancoast.co.uk]

Latest revision as of 16:36, 26 June 2026

The Variscan orogeny was a mountain-building event that gave rise to Cornwall, along with other mountain features across Europe. This was caused when the ancient continents of Euramerica and Gondwana collided to from the supercontinent of Pangaea. The granite that rose towards the surface under what is now Cornwall distilled many elements from deep in the earth into the existing 'country' rock (known in Cornwall as 'killas'), as it partially melted in the margins around the granite.

It was these areas that would very much later be mined for their wealth.

For more info, see this amazing website: [1]