As well as the numerous spoil heaps and ruined mine buildings.
Here, marine sediments - mudstones, siltstones and sandstones formed and were then buried beneath several kilometres of more recent sediment - much of which has now been eroded away by the processes of nature.
But summe menne suppose that it sesid, bycawse the wood is sore wastith.' The most important period in Cardiganshire mining was from the eighteenth century right through the nineteenth with the peak being from 1830 to 1880.
The greatest output was in 1856 when 8,560 tons of lead ore yielded 38,751 ounces of silver.
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