In this episode of Stuff You Should Know, the hosts explore the history of Doggerland, a now-submerged landmass that once connected Britain to continental Europe. The discovery of this prehistoric landscape began with fishing crews finding unusual artifacts, leading to scientific investigations that revealed evidence of human settlements, diverse wildlife, and complex environmental changes spanning thousands of years.
Using modern technology and data from oil exploration, researchers have mapped this lost world, uncovering how it transformed from tundra to forest as the climate warmed. The episode examines how various human species inhabited this region over time, and explains how rising sea levels, geological processes, and possible tsunamis gradually submerged this ancient territory beneath what is now the North Sea.

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In the late 19th century, advanced fishing technologies led to a remarkable discovery: evidence of a submerged landmass connecting the UK and Europe. When fishing crews began finding peat containing mammal bones instead of fish bones, it sparked scientific interest. Clement and Eleanor Reed proposed the existence of a land bridge after discovering submerged tree stumps and bones. This theory gained substantial support in 1931 when the trawler Kolenda discovered a 14,000-year-old antler harpoon head, confirming human habitation during the Mesolithic era.
In 1998, archaeologist Bryony Coles coined the term "Doggerland" and created the first speculative maps of this prehistoric landscape. Modern researchers like Vincent Gaffney and Simon Fitch have advanced our understanding by utilizing data from oil exploration companies. Their underwater mapping has revealed extensive evidence of settlements and artifacts, though exploration remains challenging due to heavy sediment accumulation in the North Sea.
Doggerland's environment evolved dramatically over time. During the Younger Dryas period, it was primarily tundra with grasses and shrubs. As the climate warmed, the landscape transformed into forests of birch, pine, and hazel trees. This environmental shift affected wildlife, with Ice Age species like woolly rhinoceros and mammoths giving way to temperate animals such as wild boar and beavers.
Human inhabitants also adapted to these changes. From the early Homo Antecessor nearly 800,000 years ago to the arrival of Homo sapiens around 14,000 years ago, populations evolved from hunter-gatherers to early farmers, establishing permanent settlements with advanced social organization.
Research suggests Doggerland disappeared beneath the waves between 5,000 and 7,000 years ago. The submergence resulted from a combination of factors: gradual sea-level rise following the Ice Age, isostatic rebound from melting glaciers, and potentially catastrophic tsunamis from the Storegga Slides around 8,000 years ago. According to researchers, sea levels may have risen as rapidly as one meter per century, forcing inhabitants to adapt or migrate as their homeland slowly disappeared beneath the North Sea.
1-Page Summary
The history of Doggerland provides a fascinating glimpse into a lost prehistoric world that once bridged the UK and Europe.
Discovered through the artifacts brought up by advanced fishing technologies, Doggerland was a submerged landmass in the North Sea that connected the UK and Europe. In the late 19th century, deeper fishing led to the discovery of peat, also known as "Morlog," containing mammal bones—not fish bones—indicating that the seabed might have been above water in the past.
Clement and Eleanor Reed pieced together evidence of submerged tree stumps and bones to propose that a land bridge existed, which later became known as Doggerland.
The idea gained further support when, in 1931, a trawler called the Kolenda found a chunk of peat off the coast of Norfolk that contained an eight and a half-inch harpoon head crafted from an antler, dated around 14,000 years old, affirming the time of human habitation in the Mesolithic era. Additionally, a Neanderthal skull fragment between 70,000 and 40,000 years old suggested prehistoric human presence.
Clark and Bryant viewed Doggerland not just as a land bridge but as an extensive part of the European continent, teeming with life and activity. Artifacts like a mastodon skull supported the notion that Doggerland was above sea level before it succumbed to the waters.
The Reeds' 1913 publication "Submerged Forests" was the first study to delve into the underwater woods known as Noah's Woods. Their findings alo ...
The Discovery and Early History of Doggerland
Researchers like Vincent Gaffney and Simon Fitch have furthered exploration into the submerged landscape of Doggerland, coined and initially mapped by Bryony Coles in 1998.
In 1998, archaeologist Bryony Coles published "Doggerland: A Speculative Survey," coining the term "Doggerland" after the Dogger Bank. This contagious idea suggested that Doggerland was more than just a land bridge—it was an integral part of the European continent. Coles’ work suggested that this now-submerged area was once populated with human activity, inspiring further interest in its archaeological significance.
Clark notes that Coles’ study was groundbreaking. With little information available, Coles was able to create convincing and detailed maps of Doggerland during different times it was above water, igniting curiosity and research into the area’s past.
Through the aid of underwater mapping, researchers can create more accurate landscape models of Doggerland.
Underwater mapping has revealed that the North Sea's submerged Doggerland holds significant archaeological resources like artifacts and settlements. Gaffney and graduate student Simon Fitch leveraged data obtained from oil exploration companies, notably from Petroleum Geo Services. This data, covering 23,000 square kilometers, brought to light the presence of artifacts and settlements in Doggerland, painting a picture of a lost prehistoric land.
Clark and Bryant discuss how underwater mapping has provide ...
The Scientific Research and Efforts to Study Doggerland
Doggerland, the now-submerged landmass that once connected Great Britain to continental Europe, underwent various transformations during its existence, affecting both its landscape and the species that inhabited it, including human populations.
In the Younger Dryas period, Doggerland's environment consisted primarily of a tundra landscape. Researchers determined that it was dominated by hardy vegetation like ferns, shrubs, and grasses possibly due to the samples of willow leaves, hazel, and birch found in peat deposits.
As global temperatures began to rise, the once cold and harsh tundra of Doggerland gradually transformed. Birch and pine trees started populating the area during the ensuing pre-Boreal period and the larger Holocene epoch. Later on, in the Boreal period, an even warmer climate allowed hazel to replace birch, signifying the shift to a forested environment.
With climatic shifts altering Doggerland's landscape, the animal life correspondingly evolved from Ice Age species to a more temperate array of fauna. Woolly rhinoceros, mammoths, and reindeer that thrived during the Younger Dryas had to migrate northward or became extinct as the Ice Age concluded around 11,600 years ago. Their departure made room for new inhabitants, such as wild boar, birds, otters, and beavers.
Doggerland's initial human inhabitants, Homo Antecessor, appeared nearly 800,000 years ago, followed by Neanderthals who thrived in the cold tundra, focusing on a diet rich i ...
Environmental and Ecological Characteristics of Doggerland Over Time
Doggerland, the fabled ancient land bridge once linking Britain to Europe, has long intrigued researchers with its mysterious submergence. New theories and estimates provide insight into the natural events that might have led to this area's disappearance beneath the waves.
Bryant, citing Coles, suggests that Doggerland likely disappeared around 5500 BC. The scientific consensus seems to be that Doggerland went underwater between 5000 and 7000 years ago. This timeline aligns with estimates that indicate Doggerland was fully submerged around 5,000 to 7,000 years ago, with sea levels rising gradually over hundreds of thousands of years during the aftermath of the Ice Age. The higher lands of Doggerland were slowly consumed by rising sea levels, with Dogger's Bank being one of the last areas to submerge.
Theories propose that approximately 8,000 years ago, massive tsunamis generated by submarine landslides, known as the Storegga Slides, inundated the coasts surrounding the North Sea and affected the areas making up Doggerland. Moreover, during the cold period known as the Younger Dryas, isostatic adjustment—stemming from the significant weight of glaciers and ice sheets—forced parts of the Earth's crust downward and ...
Submergence of Doggerland Theories
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