The trigger for the tsunami was a landslide named Storegga, where 3,000 cubic km of sediment collapsed in the North Sea.
"That's a lot of sediment," says Dr Hill. "Three hundred times more than all the rivers in the world hold in a year, which is what makes this event so unique. The chances of it happening again are minuscule."
The tsunami would have also reached the UK and the Imperial teams is the first study to measure its impact on British shores. Previous studies had always looked at the effect of the Storegga tsunami on the Norwegian coast.
Professor Martin Bell, head of Archaeology at Reading University, said: "What we know from the work that has been done in Doggerland is that there are major episodes of sea change around that time, of which the tsunami was the most dramatic. We know a lot about the slide itself, but the extent of the impact on east-Britain has been less studied.
There are some archaeological sites that have been flooded there. There are one or two sites in Scotland with known Mesolithic sites under layers of gravel they clearly come from the tsunami because we can tell using carbon dating."
Previously, however, two axes from Neolithic times, a period post-Storegga, had been discovered in an area of the North Sea termed the Brown Bank, which would have been affected by the tsunami.
"The axes suggest there may have been a little land surviving into the Neolithic times," says Bell. "It is difficult to prove conclusively because the land has been covered over completely... we can't just relate it to sea level change to find where those islands were."
- The Independent