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Jan
Mangerud; Martin Jakobsson; Helena Alexanderson; Valery Astakhov; Garry K. C. Clarke; Mona Henriksen; Christian Hjort; Gerhard Krinner; Juha-Pekka Lunkka; Per Möller; Andrew Murray; Olga Nikolskaya; Matti Saarnisto; John Inge Svendsen (2004).
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New constraints on the limits of the
Barents-Kara ice sheet during the Last Glacial Maximum based on borehole stratigraphy from the Pechora Sea
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and 60–50 ka, the produced ice-damming resulted in the creation of lakes and a significant rerouting of drainage in northern
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137:"Ice-dammed lakes and rerouting of the drainage of northern Eurasia during the Last Glaciation"
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The extent of the
Barents-Kara ice sheet during the Last Glacial Maximum
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The
Barents-Kara ice sheet coming and going the last 60,000 years
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in the north. In the continent, it covered from the
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42:. It is named after the seas it was centred upon:
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191:. 33rd IGC International Geological Congress.
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98:that now flow northwards.
38:which existed during the
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40:Weichselian Glaciation
32:Barents–Kara Ice Sheet
18:Barents-Kara Ice Sheet
185:Jan Mangerud (2008).
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169:. Retrieved
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52:Pechora Sea
44:Barents Sea
285:Ice sheets
279:Categories
232:glaciology
171:2010-02-25
102:References
290:Hydrology
36:ice sheet
27:Ice sheet
60:Svalbard
48:Kara Sea
206:Geology
92:Pechora
84:Yenisei
80:Eurasia
70:to the
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