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From December 2013 onwards the Somerset Levels suffered severe flooding as part of the wider 2013–2014 Atlantic winter storms in Europe and subsequent 2013–2014 United Kingdom winter floods. The Somerset Levels, or the Somerset Levels and Moors as they are less commonly but more correctly known, is a coastal plain and wetland area of ...
The 2012 Great Britain and Ireland floods had brought severe flooding to the Somerset Levels. During December 2013 and January 2014 heavy rainfall led to extensive flooding on the Somerset Levels with over 600 houses and 17,000 acres (6,900 ha) of agricultural land, including North Moor, Curry and Hay Moors and Greylake, affected.
Source: Ordnance Survey OpenData The Somerset Levels are a coastal plain and wetland area of Somerset, England, running south from the Mendips to the Blackdown Hills.. The Somerset Levels have an area of about 160,000 acres (650 km 2) and are bisected by the Polden Hills; the areas to the south are drained by the River Parrett, and the areas to the north by the rivers Axe and Brue.
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Chew Stoke Flood was a heavy rain event and severe flash flood which occurred on 10 July 1968, affecting Somerset and Southwest England in particular the Chew Valley and some areas of Bristol, notably Bedminster. [1]
The Bristol Channel floods of 30 January 1607 [a] drowned many people and destroyed a large amount of farmland and livestock during a flood in the Bristol Channel.The known tide heights, probable weather, extent and depth of flooding, and coastal flooding elsewhere in the British Isles on the same day all point to the cause being a storm surge rather than a tsunami.