Red Screes - Geology and Mining

Geology and Mining

Drift deposits overlie the dacitic welded lapilli-tuff and sandstone of the Lincomb Tarns Formation.

There is evidence of mining in Caiston Glen, with the mouth of a level opening about halfway up the beck. This was an unsuccessful trial for lead and extends about 80 ft into the fellside. There is a further small working nearby. There are also the remains of a trial for copper on the eastern flank, a 120 ft level being driven into the fell from close to the modern road.

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    Any relation to the land, the habit of tilling it, or mining it, or even hunting on it, generates the feeling of patriotism. He who keeps shop on it, or he who merely uses it as a support to his desk and ledger, or to his manufactory, values it less.
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