Barents–Kara Ice Sheet

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The Barents–Kara Ice Sheet was a vast Pleistocene ice mass that covered the Barents and Kara seas and adjacent Arctic continental areas during the last ice age.

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Statements (47)

Predicate Object
instanceOf Pleistocene ice sheet
glacial ice mass
affected ocean circulation in the Arctic gateway
paleoclimate of the Eurasian Arctic
category Pleistocene glaciations
Quaternary geology of the Arctic
covered Barents Sea shelf NERFINISHED
Franz Josef Land NERFINISHED
Kara Sea shelf NERFINISHED
Novaya Zemlya NERFINISHED
Svalbard region NERFINISHED
adjacent Arctic continental margin
parts of northern Russia
disappearedBy early Holocene
evidenceFrom multibeam bathymetry
sediment cores
seismic reflection data
existedDuring Last Glacial Maximum NERFINISHED
extent over Barents and Kara seas and adjacent land areas
formedBy glacial accumulation
snowfall and ice compaction
hasPart Barents sector NERFINISHED
Kara sector
influenced Quaternary sedimentation on the Barents shelf
glacial isostatic adjustment in the Barents Sea region
relative sea-level changes in the Eurasian Arctic
leftBehind glacial landforms on the Barents Sea floor
moraines
leftBehind glacial lineations
till deposits
tunnel valleys
locatedIn Arctic Ocean region
Barents Sea NERFINISHED
Eurasian Arctic NERFINISHED
Kara Sea NERFINISHED
marginsReached continental shelf edge in parts of the Barents Sea
outer Kara Sea shelf in some sectors
partOf Eurasian Ice Sheet Complex NERFINISHED
Last Glacial Maximum cryosphere NERFINISHED
relatedTo British–Irish Ice Sheet NERFINISHED
Fennoscandian Ice Sheet NERFINISHED
retreatedDuring late Pleistocene deglaciation
studiedBy Quaternary science
glacial geology
marine geophysics
temporalExtent Pleistocene epoch
thickness over 1 kilometer in places

Referenced by (2)

Full triples — surface form annotated when it differs from this entity's canonical label.

Last Glacial Maximum hasMajorIceSheet Barents–Kara Ice Sheet
Northern Hemisphere ice sheets included Barents–Kara Ice Sheet