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The Barents–Kara Ice Sheet was an ice sheet which existed during the Weichselian Glaciation. It is named after the seas it was centred upon: Barents Sea and Kara Sea. The ice sheet covered the Pechora Sea, the southeastern part of the Barents Sea, Novaya Zemlya and the Kara Sea, likely reaching up to Svalbard and Franz Joseph Land in the north. In the continent, it covered from the North Russian Plain to the North Siberian Lowland.During the periods 90–80 ka and 60–50 ka, the produced ice-damming resulted in the creation of lakes and a significant rerouting of drainage in northern Eurasia, including the major rivers Yenisei, Ob, Pechora and Mezen that now flow northwards.

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  • Barents-Kara-Eisschild (de)
  • Barents–Kara Ice Sheet (en)
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  • The Barents–Kara Ice Sheet was an ice sheet which existed during the Weichselian Glaciation. It is named after the seas it was centred upon: Barents Sea and Kara Sea. The ice sheet covered the Pechora Sea, the southeastern part of the Barents Sea, Novaya Zemlya and the Kara Sea, likely reaching up to Svalbard and Franz Joseph Land in the north. In the continent, it covered from the North Russian Plain to the North Siberian Lowland.During the periods 90–80 ka and 60–50 ka, the produced ice-damming resulted in the creation of lakes and a significant rerouting of drainage in northern Eurasia, including the major rivers Yenisei, Ob, Pechora and Mezen that now flow northwards. (en)
  • Der Barents-Kara-Eisschild war ein massiver Eisschild in Nord-Russland, dessen größte Ausdehnung in der Weichseleiszeit vor etwa 90.000 Jahren bestand. Damals bedeckte der Eisschild die , den südöstlichen Teil der Barentssee, die Doppelinsel Nowaja Semlja, die Karasee und reichte im Norden möglicherweise bis Spitzbergen und Franz-Joseph-Land. Auf dem Festland lag das Gebiet vom Nordrussischen Tiefland bis ins Nordsibirische Tiefland ebenfalls unter dem Eisschild. (de)
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  • Der Barents-Kara-Eisschild war ein massiver Eisschild in Nord-Russland, dessen größte Ausdehnung in der Weichseleiszeit vor etwa 90.000 Jahren bestand. Damals bedeckte der Eisschild die , den südöstlichen Teil der Barentssee, die Doppelinsel Nowaja Semlja, die Karasee und reichte im Norden möglicherweise bis Spitzbergen und Franz-Joseph-Land. Auf dem Festland lag das Gebiet vom Nordrussischen Tiefland bis ins Nordsibirische Tiefland ebenfalls unter dem Eisschild. Bei späteren Vorstoßphasen des Eises in der Weichseleiszeit erreichte es wahrscheinlich nicht mehr das russische Festland, während der Fennoskandische Eisschild im Westen immer größere Gebiete bedeckte und vor etwa 20.000 Jahren sein Maximum erreichte. Es wird angenommen, dass der Eisschild den Abfluss großer russischer Flüsse (Petschora, Ob und Jenissei) in den Arktischen Ozean verhinderte und mehrere Seen sich aufstauten. Es wird vermutet, dass im Westsibirischen Tiefland der flache, riesige Westsibirische Gletschersee entstand, der in den Aralsee oder ins Kaspische Meer entwässerte. (de)
  • The Barents–Kara Ice Sheet was an ice sheet which existed during the Weichselian Glaciation. It is named after the seas it was centred upon: Barents Sea and Kara Sea. The ice sheet covered the Pechora Sea, the southeastern part of the Barents Sea, Novaya Zemlya and the Kara Sea, likely reaching up to Svalbard and Franz Joseph Land in the north. In the continent, it covered from the North Russian Plain to the North Siberian Lowland.During the periods 90–80 ka and 60–50 ka, the produced ice-damming resulted in the creation of lakes and a significant rerouting of drainage in northern Eurasia, including the major rivers Yenisei, Ob, Pechora and Mezen that now flow northwards. (en)
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