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Post-glacial rebound
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Post-glacial rebound is the rise of land masses after the removal of the huge weight of ice sheets during the last glacial period, which had caused isostatic depression. Post-glacial rebound and isost
This layered beach at Bathurst Inlet, Nunavut is an example of post-glacial rebound after the last Ice Age. Little to no tide helped to form its layer
This layered beach at Bathurst Inlet, Nunavut is an example of post-glacial rebound after the last Ice Age. Little to no tide helped to form its layer-cake look. Isostatic rebound is still underway here.
Changes in the elevation of Lake Superior due to glaciation and post-glacial rebound
Changes in the elevation of Lake Superior due to glaciation and post-glacial rebound
Doggerland
Videos
Doggerland was a large area of land in Northern Europe, now submerged beneath the southern North Sea. This region was repeatedly exposed at various times during the Pleistocene epoch due to the loweri
Post-glacial rebound
…shelves were exposed and many islands became connected with the continents through dry land. This was the case between the British Isles and Europe (Doggerland), or between Taiwan, the Indonesian islands and Asia (Sundaland). A land bridge also existed between Siberia and Alaska that allowed the migration of…
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
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)
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