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What glaciers left behind in the post-ice age in Scandinavia
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At the end of the last ice age, there was a time when glaciers reached their maximum. This period is called the Last Glacial Maximum, or LGM. After the LGM, glaciers melt over thousands of years. As a result, many changes have taken place in Fennoscandia.
This episode introduces the Fennoscandia ice sheet's thawing and the first Scandinavians' migration. It also introduces the uplift, the tsunami, and the formation of lakes caused by deglaciation.
00:18 Introduction of Fennoscandia
01:28 What happens when glaciers melt
03:29 Evidence of terminal moraine
04:15 Countries in Fennoscandia
06:16 Deglaciation and migration of first Scandinavians
10:20 Land uplift
12:58 Changes in the Baltic Sea since the Ice Age
Papers Referenced:
Population genomics of Mesolithic Scandinavia: Investigating early postglacial migration routes and high-latitude adaptation
#fennoscandia #iceage #lgm #ancienthistory #ancientstory
This episode introduces the Fennoscandia ice sheet's thawing and the first Scandinavians' migration. It also introduces the uplift, the tsunami, and the formation of lakes caused by deglaciation.
00:18 Introduction of Fennoscandia
01:28 What happens when glaciers melt
03:29 Evidence of terminal moraine
04:15 Countries in Fennoscandia
06:16 Deglaciation and migration of first Scandinavians
10:20 Land uplift
12:58 Changes in the Baltic Sea since the Ice Age
Papers Referenced:
Population genomics of Mesolithic Scandinavia: Investigating early postglacial migration routes and high-latitude adaptation
#fennoscandia #iceage #lgm #ancienthistory #ancientstory
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