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During the Weichselian glaciation, almost all of Scandinavia was buried beneath a thick permanent sheet of ice and the Stone Age was delayed in this region.Some valleys close to the watershed were indeed ice-free around 30 000 years B.P. Coastal areas were ice-free several times between 75 000 and 30 000 years B.P. and the final expansion towards the late Weichselian maximum took place after ...
Scandinavian Journal of History; List of Scandinavian saints; Second Northern War and Norway; Skilling (currency) Socken; Stone circle (Iron Age) Stone ship; Stortorget, Malmö; Siege of Fredrikstad; Swedish–Norwegian War; Swedish–Norwegian War (1099–1101)
The history of Sweden can be traced back to the melting of the Northern Polar Ice Caps.From as early as 12000 BC, humans have inhabited this area. Throughout the Stone Age, between 8000 BC and 6000 BC, early inhabitants used stone-crafting methods to make tools and weapons for hunting, gathering and fishing as means of survival. [1]
The Nordic Stone Age refers to the Stone Age of Scandinavia. During the Weichselian glaciation (115,000 – 11,700 years ago), almost all of Scandinavia was buried beneath a thick permanent ice cover, thus, the Stone Age came rather late to this region. As the climate slowly warmed up by the end of the ice age, nomadic hunters from central ...
Galdhøpiggen is the highest point in Scandinavia and is a part of the Scandinavian Mountains.. The geography of Scandinavia is extremely varied. Notable are the Norwegian fjords, the Scandinavian Mountains covering much of Norway and parts of Sweden, the flat, low areas in Denmark and the archipelagos of Finland, Norway and Sweden.
Scandinavia was formally Christianized by 1100 AD. The period 1050 to 1350—when the Black Death struck Europe—is considered the Older Middle Ages. The Kalmar Union between the Scandinavian countries was established in 1397 and lasted until King Gustav Vasa ended it upon seizing power during the Swedish War of Liberation, which concluded in ...
The pre-history of Scandinavia begins at the end of the Pleistocene epoch, following the last glacial period's receding Fenno-Scandian ice sheet. Parts of Denmark, Scania and the Norwegian coast line were free from ice around 13,000 BC, and around 10,000 BC the rim of ice was around Dalsland, Västergötland and Östergötland.
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