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3 Maps Of Doggerland: Mapping The Lost World

Last Updated: February 7, 2025 Leave a Comment

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Excerpt of Map of Doggerland - The Europe That Was

Excerpt of Full Map by William E. McNulty and Jerome N. Cookson, National Geographic Magazine (click for full version)
The map above shows how big Doggerland may have been at it’s maximum extent in around 16,000 BC (18,000 years ago).

For more please see the following:

Doggerland was a vast area of land that once connected Great Britain to continental Europe during and after the last Ice Age.

Here’s an overview of its history:

What Was Doggerland?

  • A Prehistoric Landscape:
    Doggerland was a rich, marshy landscape that served as a bridge between Britain and mainland Europe. It provided a haven for diverse wildlife and early human communities, who took advantage of its abundant natural resources for hunting, foraging, and eventually, settlement.

Did people live on Doggerland?

Yes, people did live on Doggerland. Here’s a detailed look at the evidence and context:

  • Mesolithic Hunter-Gatherers:
    Doggerland was inhabited by Mesolithic (Middle Stone Age) hunter-gatherer communities. These groups occupied the region for several thousand years, taking advantage of its rich resources such as rivers, lakes, and coastal environments.
  • Rich Ecosystems:
    The varied landscapes of Doggerland—including wetlands, woodlands, and open plains—provided abundant food sources like fish, shellfish, wild game, and edible plants. This diversity made it an ideal habitat for mobile, resourceful groups who relied on seasonal movements and a deep knowledge of their environment.
  • Archaeological Evidence:
    Although Doggerland is now submerged under the North Sea, archaeological surveys (including underwater excavations and dredging) have uncovered tools, flint implements, and animal remains. These finds indicate that humans not only lived there but also moved through the region, likely using it as a corridor between what is now Britain and continental Europe.

How Was It Formed?

  • Glacial Influences and Lower Sea Levels:
    During the peak of the last Ice Age in 20,000 BC (roughly 22,000 years ago), much of the world’s water was locked up in massive ice sheets. This caused global sea levels to drop significantly, exposing large areas of what is now the North Sea. Doggerland emerged as a broad expanse of land featuring river valleys, wetlands, and forests.
  • Geological Shaping:
    The interplay of glacial sculpting, sediment deposition, and subsequent isostatic (land-surface) adjustments played a key role in shaping this landscape, making it a dynamic environment over thousands of years.

Map of Doggerland from the present day all the way back to 115,000 BC

Map created by Francis Lima
The map above shows what the area looks like today, from the geographical situation in 2000 (furthest left) to 18,000 years ago (middle) to the late years of the Vistula-Würm Glaciation (furthest right).

How and Why Did It Disappear?

  • Rising Sea Levels:
    As the climate warmed at the end of the Ice Age, the ice sheets began to melt. The resulting rise in sea levels was gradual at first but eventually accelerated, inundating Doggerland.
  • Final Inundation:
    By around 8,000 years ago, continued sea-level rise, possibly combined with periodic storm surges, transformed Doggerland from a habitable landscape into the shallow, submerged seabed of today’s southern North Sea (see below).

Doggerland Tsunami?

The “Doggerland tsunami” was a potentially massive tsunami associated with the Storegga Slide—a submarine landslide off the coast of Norway that occurred around 8,150 years ago (roughly 6,200 BCE).

Here’s what is known about the event and its context:

The Storegga Slide and Its Tsunami

  • What Happened:
    The Storegga Slide was a huge underwater landslide in the Norwegian Sea. When a large volume of sediment suddenly moved, it displaced a massive amount of water, generating a tsunami that radiated across the North Atlantic and North Sea.
  • Impact on the Region:
    The tsunami is estimated to have reached significant heights along various coastlines. Modeling studies suggest that, while the tsunami was most intense along the Norwegian coast, its waves also impacted the shallow areas of the North Sea—including Doggerland—with wave heights that may have been on the order of several meters.
  • Role of the Tsunami:
    The tsunami generated by the Storegga Slide is thought to have caused sudden and dramatic flooding in parts of Doggerland. While rising sea levels over centuries were the primary driver behind Doggerland’s eventual submergence, the tsunami would have delivered a sudden, catastrophic pulse of water that likely disrupted local ecosystems and may have forced some communities to relocate. There is ongoing scientific discussion about the extent of the tsunami’s damage; some researchers propose that it was a significant stressor on the inhabitants, while others suggest that its impact, though dramatic, was relatively localized compared to the long-term effects of sea-level rise.

Scientific Insights

  • Geological Evidence:
    Sediment deposits and other geological records in the North Sea region provide evidence for the Storegga Slide tsunami. These deposits help scientists reconstruct the event’s timing, magnitude, and impact on coastal regions, including Doggerland.
  • Modeling and Research:
    Computer simulations and physical models of the tsunami have been used to estimate wave heights and inundation areas. While there remains some debate about the precise effects, the consensus is that the tsunami contributed to the environmental changes that eventually rendered Doggerland uninhabitable.

What’s left of Doggerland today?

Today, Doggerland exists only as a submerged landscape beneath the North Sea.

Here’s what that means in practical terms:

  1. Submerged Landmass:
    The once vast land bridge that connected Britain to continental Europe is now entirely underwater. What remains is the geological footprint of Doggerland—its sediment layers, ancient river channels, and topographical features—mapped out on the seabed.
  2. The Dogger Bank:
    One of the most notable remnants is the Dogger Bank, a relatively shallow area of the North Sea. While not “land” in the traditional sense (it’s underwater), the Dogger Bank is considered a key feature of what was once Doggerland. It’s an important area for marine life and has also been a focus of geological and archaeological research.
  3. Archaeological and Geological Evidence:
    Although there are no standing structures or visible settlements today, researchers have uncovered evidence of Doggerland’s past through:

    • Sediment Cores and Seismic Surveys: These help reconstruct the ancient landscape and understand the changes that occurred as sea levels rose.
    • Underwater Artifacts: Occasionally, tools, bones, and other relics of Mesolithic communities are found, often by fishermen or through dedicated underwater archaeological projects. These finds provide clues about the people who once lived there.
  4. Ongoing Research:
    Advances in underwater mapping and remote sensing technology have allowed scientists to better visualize and understand Doggerland’s submerged landscape. This research not only tells us about the natural history of the region but also about the human history of migration, adaptation, and cultural change in prehistoric Europe.

And finally here is the area of the Dogger Bank (the last remains of Doggerland) today.

Doggerbank

Further Reading and Research Projects

Here are some links to articles and projects for a deeper dive into Doggerland:

  • Searching for Doggerland (National Geographic) An engaging piece that covers how rising seas transformed a once-thriving region into an underwater mystery, and how scientists figured it all out.
  • Hidden Doggerland underworld uncovered in North Sea (BBC) This article explores the history of Doggerland and discusses the latest scientific findings about this submerged landscape.
  • Europe’s Lost Frontiers (Academic) – Project to map Doggerland.
  • North Sea Palaeolandscape Project – Ran from 2005 – 2006 and sought to utilise existing 3D seismic data to generate information on the Mesolithic Landscape of the North Sea.

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