Sea levels were 120–135 m lower during the last glacial maximum, exposing Doggerland as a habitable land bridge between Britain and Europe. Around 8,150 years ago, the Storegga submarine landslide off Norway displaced about 200 km³ of sediment and triggered a tsunami that reached Scotland and Shetland. Near Inverness, a Mesolithic occupation layer with worked flint was buried beneath tsunami sand; no structures survived. Some researchers argue the event helped end permanent habitation on Doggerland. 🌊
Doggerland: Lost land bridge hit by Storegga tsunami around 8,150 years ago

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Key facts
- At the last glacial maximum, about 20,000 years ago, global sea level was roughly 120–135 m below present.
- Meltwater pulse 1A, around 14,500 years ago, raised sea level by as much as about 20 m over a few centuries.
- Doggerland was a habitable land bridge between Britain and continental Europe; Beringia connected Asia and North America.
- Around 8,150 years ago, the Storegga submarine landslide off Norway displaced about 200 km³ of sediment and generated a major tsunami.
- Moss Hylocomium splendens fragments retaining chlorophyll, together with their growth patterns, constrained the tsunami's timing and showed that some moss was torn up alive and rapidly buried.
- The tsunami reached Scotland and Shetland, both west of the Storegga source region.
- Near Inverness, a Mesolithic occupation layer with worked flint was found beneath sand attributed to the Storegga tsunami; no structures survived.
- Some researchers have suggested that the tsunami may have ended permanent habitation on Doggerland; this remains a hypothesis rather than an established conclusion.
Sources
abc.net.au
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bbc.com
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kathmandupost.com
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english.cas.cn
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abc.net.au
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english.cctv.com
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kathmandupost.com
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Past sea levelen.wikipedia.org
Low levels were reached during the Last Glacial Maximum (LGM), about 20,000 years ago. The last time the sea level was higher than today was during the Eemian, ...
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