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The entire wiki reimagined as a visual magazine with video discovery · Watch your interests come alive
Situation of the southern North Sea during Marine Isotope Stages (MIS) 25-21 (c. 1 million-800,000 years ago) MIS 17 (c. 700,000 years ago), MIS 12 (Anglian) glaciation (c. 480-425,000 years ago) and MIS 11 (Hoxnian) interglacial (c. 425-375,000 years ago)
Situation of the southern North Sea during Marine Isotope Stages (MIS) 25-21 (c. 1 million-800,000 years ago) MIS 17 (c. 700,000 years ago), MIS 12 (A
Paleogeography of the southern North Sea during Marine Isotope Stages (MIS) 19-13 (c. 800,000-480,000 years ago) during episodes of high (left) and lo
Paleogeography of the southern North Sea during Marine Isotope Stages (MIS) 19-13 (c. 800,000-480,000 years ago) during episodes of high (left) and low (right) sea level
The red line marks Dogger Bank, which is most likely a moraine formed in the Pleistocene
The red line marks Dogger Bank, which is most likely a moraine formed in the Pleistocene
A Woolly mammoth skull discovered by fishermen in the North Sea, at the Celtic and Prehistoric Museum, Ireland
A Woolly mammoth skull discovered by fishermen in the North Sea, at the Celtic and Prehistoric Museum, Ireland
The yellow numbers give the height of the tsunami wave as indicated by tsunamites studied by researchers.
The yellow numbers give the height of the tsunami wave as indicated by tsunamites studied by researchers.
Storegga tsunami deposits (grey upper layer), bracketed by peat (dark brown layers), taken at Maryton on the Montrose Basin, Scotland
Storegga tsunami deposits (grey upper layer), bracketed by peat (dark brown layers), taken at Maryton on the Montrose Basin, Scotland