Geology
The larger part of the island is formed from highly faulted and folded sedimentary rocks of Ordovician age. There is a belt of younger Silurian rocks along the west coast between Niarbyl and St Patrick's Isle and a small area of Devonian sandstones around Peel. A band of Carboniferous age rocks underlies part of the northern plain but is nowhere seen at the surface however similar age rocks do outcrop in the south between Castletown, Silverdale and Port St Mary. Permo-Triassic age rocks are known to lie beneath Point of Ayre but, as with the rest of the northern plain, these rocks are concealed by substantial thicknesses of superficial deposits.
The island has significant deposits of copper, lead and silver, zinc, iron, and plumbago (a mix of graphite and clay). There are also quarries of black marble, limestone flags, clay schist, and granite. These are all modern, and there was no noticeable exploitation of metals or minerals prior to the modern era.
Read more about this topic: Geography Of The Isle Of Man