Tsunamis affecting the British Isles
Tsunamis affecting Britain and Ireland are extremely uncommon, and there have only been two confirmed cases in recorded history. Meteotsunamis are somewhat more common, especially on the southern coasts of England around the English and Bristol Channels.
Confirmed tsunamis
Scotland (6100 BC)
The east coast of Scotland was struck by a high tsunami around 6100 BC, during the Mesolithic period. The wave was caused by the massive underwater Storegga slide off Norway. The tsunami even washed over some of the Shetland Islands. Tsunamite dating from this event can be found at various locations around the coastal areas of Scotland, and are also a tourist feature in the Montrose Basin, where there is a layer of deposited sand about thick.At the time, what became the east coast of England was connected to the areas of Denmark and the Netherlands by a low-lying land bridge, now known to archaeologists as Doggerland. The area is believed to have had a coastline of lagoons, marshes, mudflats, and beaches, and may have been the richest hunting, fowling, and fishing ground in Europe at the time. Much of this land would have been inundated by the tsunami, with a catastrophic impact on the local human population.
Lisbon earthquake (1755)
The coast of Cornwall was hit by a high tsunami on 1 November 1755, at around 14:00. The waves were caused by the 1755 Lisbon earthquake. The tsunami took almost four hours to reach the UK. The tsunami was also observed along the south coast of England and on the River Thames in London. Contemporary reports say that there were three of these tsunami waves, and that the sea receded very quickly, then rose up. At St Michael's Mount, the sea rose suddenly and then retired; ten minutes later, it rose very rapidly, then ebbed equally rapidly. The sea rose in Penzance and at Newlyn; the same effect was reported at St Ives and Hayle. Although there is no record of the overall death toll, the 19th-century French writer Arnold Boscowitz claimed that "great loss of life and property occurred upon the coasts of Cornwall".The tsunami also reached Galway in Ireland, at a height of, and caused some serious damage to the "Spanish Arch" section of the city wall.
There are also historical records of the tsunami reaching Pembrokeshire and washing up the Cleddau estuary.
Lisbon earthquake (1761)
At Mount's Bay in Cornwall, a small tsunami up to 1.9 meters was observed following the 1761 Portugal earthquake.Meteotsunami (1929)
On 20 July 1929 a wave reported as being between high struck the south coast of England including busy tourist beaches at Worthing, Brighton, Hastings and Folkestone. Two people drowned and the wave was attributed to a squall line travelling along the English Channel.South coast (2011)
A small tsunami in the English Channel with a peak wave height anomaly of occurred on 29 June 2011 affecting four counties on the south coast of England; Cornwall, Devon, Dorset and Hampshire. The tsunami was described as mild and there were no records of injuries or damage. Video footage clearly showed the tsunami and there were reports of fish leaping out the water and hair lifting up because of a static charge. Initial media speculation attributed the event to an underwater landslide, as no earthquakes were recorded at the time. However, the British Geological Survey concluded that it was unlikely to have been caused by a submarine landslide and was probably a meteotsunami.Possible tsunamis
Orkney and Shetland (3500 BC)
Traces of a tsunami called the Garth tsunami have been reported from the Shetland Islands. The tsunami took place 5,500 years ago and may be connected to the presence of mass burials on both the Shetland and Orkney islands.England and Wales (1014)
A widespread flood was reported in the Anglo-Saxon Chronicle to have occurred in Britain, from the coast of Cumbria to Kent, on 28 September 1014. William of Malmesbury stated that "A tidal wave... grew to an astonishing size such as the memory of man cannot parallel, so as to submerge villages many miles inland and overwhelm and drown their inhabitants." The event was also mentioned in Welsh bardic chronicles. Accounts suggest that a flood affected Kent, Sussex, Hampshire, Cumbria, and Mount's Bay in Cornwall, where the Bay was "inundated by a 'mickle seaflood' when many towns and people were drowned".Dover Straits earthquake (1580)
On 6 April 1580 there was a 5.8 magnitude earthquake with its epicentre on the sea bed close to Calais. Giant waves were reported, and hundreds of people were killed when ships were sunk by the waves and the low-lying coastal land around Calais was inundated by the sea. In Dover, part of the chalk cliff collapsed, taking with it part of Dover Castle.A contemporary French account states: "in the city of Calais such a horrible and terrible earthquake came to pass that a great part of the houses fell, and even the sea overflowed into the city and did ruin and drown a great number of houses, and numerous persons perished, and a great multitude of beasts lost which were at pasture outside this city."
In recent years, it has been suggested that these waves were a tsunami and not seiches. It is unlikely that the earthquake alone was strong enough to rupture the sea bed to trigger a tsunami, but it appears to have been sufficiently powerful to have caused an undersea landslide that was capable of generating a tsunami, as happened in Papua New Guinea in 1998, killing around 2,500 people.