SCIENTISTS led by the University of Bradford have made a major breakthrough in the hunt for confirmation of a historic mega tsunami that is thought to have raged across the North Sea some 8,000 years ago.

The gigantic waves are thought to have decimated the Stone Age peoples living in the area between the UK and mainland Europe which at the time was dry land and dubbed Doggerland after the Dogger Bank area of sandbanks.

Evidence of the catastrophic event has already been found in onshore sediments in Western Scandinavia, the Faroe Isles, northeast Britain, Denmark and Greenland but now for the first time confirmation of the event has been found on the UK’s southern coasts.

The giant tsunami, known as the Storegga Slide, was caused when an area of seabed the size of Scotland measuring some 80,000sq km and around 3,200 cubic km shifted suddenly off the coast of Norway.

Bradford Telegraph and Argus: A graphic showing where the tsunami hit Doggerland and the UK coastA graphic showing where the tsunami hit Doggerland and the UK coast

Professor Vince Gaffney from the School of Archaeological and Forensic Sciences in the Faculty of Life Sciences at the University of Bradford said: “Exploring Doggerland, the lost landscape underneath the North Sea, is one of the last great archaeological challenges in Europe.

"This work demonstrates that an interdisciplinary team of archaeologists and scientists can bring this landscape back to life and even throw new light on one of prehistory’s great natural disasters, the Storegga tsunami.

“The events leading up to the Storegga tsunami have many similarities to those of today. Climate is changing and this impacts on many aspects of society, especially in coastal locations.”

Bradford Telegraph and Argus: Professor Vince GaffneyProfessor Vince Gaffney

Details of the discoveries, carried out by the Europe’s Lost Frontiers European Research Council-funded research consortium, have been published in the journal Geosciences.

The research was led by the University of Bradford and involved Universities of Warwick, Wales St Trinity David, St Andrews, Cork, Aberystwyth, Tartu as well as the Smithsonian and Natural History Museum.

It is thought the tsunami, the largest to hit Northern Europe since the end of the last ice age, happened following a period of global climate change. Until now no clear trace of the tsunami had been found across the southern North Sea and importantly no trace had been found on Doggerland, which was gradually swallowed by rising sea levels after the end of the last glacial maximum. Indeed, scientists now think the tsunami may even have led to the final inundation of Doggerland.

Cores from an area south of a marine trough named the Outer Dowsing Deep provided nearly half a metre of tsunami-like deposits, stones and broken shells sandwiched between laminated estuarine sediments.

Dating indicated they were contemporary with the Storegga event, while analysis including geochemical, sedimentological, palaeomagnetic, isotopic, palaeobotany and ‘sedaDNA’ (sedentary DNA) techniques showed the deposits could be readily interpreted as resulting from a tsunami.

The multi-proxy characterisation was necessary as the signatures of tsunamis are often difficult to identify in comparison to those from periodic storm activity. Key to understanding the sequence was the interpretation of geochemical signatures of three major waves hitting and retreating from the land.

Scientists at the University of Bradford have already provided much ground-breaking research into Doggerland and mapping techniques have enabled them to identify the landscape of what has been called "Britain's Atlantis" with rivers, lakes, hills and coastlines identified in a country which had previously been a heartland of human occupation in Europe.

Doggerland was first identified as a lost landscape over a century ago, with trawlers occasionally netting archaeological remains, including a woolly mammoth skull.

At the time the tsunami hit Doggerland, a Mesolithic hunter-gather people could have been using the remaining archipelago and for those unfortunate enough to be caught within the tsunami run-up zone, it would have been devastating. However, the palaeo-topography and environmental modelling suggests that much of the landscape may have survived reasonably intact to rapidly return to pre-tsunami conditions.

The longer term fate of these lands was to be submerged as sea level rose to those of the present day.