UK

The Irish Ice Sheet

By Dr Sam Roberson, British Geological Survey, Belfast Glaciation of Ireland during the Devensian The island of Ireland has been glaciated many times during the Quaternary period.  The last glaciation in Ireland is referred to historically as the ‘Midlandian’, but now, the British-Irish term ‘Devensian’ is more commonly used. During the Devensian, the British-Irish Ice …

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Last Glacial Maximum

The British-Irish Ice Sheet reached its most recent maximum extent around 27,000 years ago. It was drained by many fast-flowing ice streams, and reached the edge of the continental shelf around its northern border. In the south, it terminated near the Vale of York, with a lobe penetrating down the eastern coastline as far as …

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Glacial erratics

What is a glacial erratic? Glacial erratics, often simply called erratics, or erratic boulders, are rocks that have been transported by ice and deposited elsewhere. The type of rock (lithology) that the glacial erratic is made from is different to the lithology of the bedrock where the erratic is deposited. For example, an erratic could …

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British-Irish Ice Sheet

Other relevant articles Glacial Cirques in Snowdonia Upland Cirque Glacier Landsystem in Britain Alpine Icefield landsystem of upland Britain Plateau Icefield Landsystem of the UK Glacial erratics Videos This GIF shows the evolution of the Scandinavian Ice Sheet (of which Britain was a part). This animation is based on an ice-sheet reconstruction using glacial geomorphology …

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