Overview of the geology of the isle of Anglesey, Wales
The geology of Anglesey, the largest (714 km2) island in Wales is some of the most complex in the country. Anglesey has relatively low relief, the 'grain' of which runs northeast–southwest, i.e. ridge and valley features extend in that direction reflecting not only the trend of the late Precambrian and Palaeozoic age bedrock geology but also the direction in which glacial ice traversed and scoured the island during the last ice age. It was realised in the 1980s that the island is composed of multiple terranes, recognition of which is key to understanding its Precambrian and lower Palaeozoic evolution. The interpretation of the island's geological complexity has been debated amongst geologists for decades and recent research continues in that vein.[1][2]
^Campbell, Stewart; Wood, Margaret; Windley, Brian (2014). Footsteps through Time: The Rocks and Landscape of Anglesey Explained (First ed.). GeoMon, Isle of Anglesey County Council. p. vi.
^British Geological Survey 1:625,000 scale geological map Bedrock Geology UK South 5th Edn. NERC 2007
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