Several times during the Last Ice Age, the ice sheet covered only mountain areas so that it theoretically was possible for humans to colonize coastal areas of Norway. The last time this happened prior to the Last Glacial Maximum (LGM: 26,000–19,000 years ago) was during the Ålesund Interstadial, 38,000–34,000 years ago. However, no traces of human presence have been found from these ice-free intervals. Following the LGM, it was not until the Bølling Interstadial (14,700–14,000 years ago) that ice-free areas were large enough to host a potentially permanent human population. Some archaeologists previously considered that people arrived at the west coast of Norway this early, but most scientists now reject this hypothesis. An ice sheet margin...
The relative sea level rose 10 m on Sotra, western Norway, during the Younger Dryas (YD). Based on d...
The margins of the Fennoscandian Ice Sheet (FIS) during the Last Glacial Maximum (LGM) are fairly we...
Current warming in the Arctic is occurring at a rate two to three times higher than that of the rest...
Several times during the Last Ice Age, the ice sheet covered only mountain areas so that it theoreti...
Recent work has suggested that the Scandinavian ice sheet was much more dynamic than previously beli...
Previous assumptions of continuous ice cover of the core area of the Fennoscandian Ice Sheet, from M...
The first men to appear in what is now Norway, emerged from dim prehistory when the great inland ice...
This article contributes a western Scandinavian perspective to the discussion of the human coloniza...
The thinning and final decay of the Scandinavian Ice Sheet in the Gudbrandsdalen area in central sou...
Recent work suggests an emerging new paradigm for the Scandinavian ice sheet (SIS); one of a dynamic...
Understanding past responses of ice sheets to climate change provides an important long-term context...
Reconstructions of postglacial relative sea level history in formerly glaciated terrains reflect the...
Summary of the thesis For more than 11,000 years ago, human groups entered and utilized territories...
Nordic countries have experienced multiple glaciations and intervening interglacials during the last...
Andøya on the NW coast of Norway is a key site for understanding the Last Glacial Maximum (LGM) in n...
The relative sea level rose 10 m on Sotra, western Norway, during the Younger Dryas (YD). Based on d...
The margins of the Fennoscandian Ice Sheet (FIS) during the Last Glacial Maximum (LGM) are fairly we...
Current warming in the Arctic is occurring at a rate two to three times higher than that of the rest...
Several times during the Last Ice Age, the ice sheet covered only mountain areas so that it theoreti...
Recent work has suggested that the Scandinavian ice sheet was much more dynamic than previously beli...
Previous assumptions of continuous ice cover of the core area of the Fennoscandian Ice Sheet, from M...
The first men to appear in what is now Norway, emerged from dim prehistory when the great inland ice...
This article contributes a western Scandinavian perspective to the discussion of the human coloniza...
The thinning and final decay of the Scandinavian Ice Sheet in the Gudbrandsdalen area in central sou...
Recent work suggests an emerging new paradigm for the Scandinavian ice sheet (SIS); one of a dynamic...
Understanding past responses of ice sheets to climate change provides an important long-term context...
Reconstructions of postglacial relative sea level history in formerly glaciated terrains reflect the...
Summary of the thesis For more than 11,000 years ago, human groups entered and utilized territories...
Nordic countries have experienced multiple glaciations and intervening interglacials during the last...
Andøya on the NW coast of Norway is a key site for understanding the Last Glacial Maximum (LGM) in n...
The relative sea level rose 10 m on Sotra, western Norway, during the Younger Dryas (YD). Based on d...
The margins of the Fennoscandian Ice Sheet (FIS) during the Last Glacial Maximum (LGM) are fairly we...
Current warming in the Arctic is occurring at a rate two to three times higher than that of the rest...