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Record #150065:

Maximum extent of the Eurasian ice sheets in the Barents and Kara Sea region during the Weichselian / John Inge Svendsen, and 13 others.

Title: Maximum extent of the Eurasian ice sheets in the Barents and Kara Sea region during the Weichselian / John Inge Svendsen, and 13 others.
Author(s): Svendsen, John Inge.
Date: 1999.
In: Boreas. (1999.), Vol. 28(1) (1999)
Abstract: Presents preliminary reconstruction of maximum ice-sheet extent during Early/Middle Weichselian (before 50,000 yr BP) and during Late Weichselian (about 20,000-18,000 yr BP). States Early/Middle Weichselian ice sheets were much larger than those of Late Weichselian glacial maximum, concluding that Grosswald's theory is incorrect in depicting ice sheets that are much too large. Theory given by authors allows for half size of Grosswald's reconstruction of ice-sheet extent in Eurasian Arctic in Late Weichselian. Concludes Russian mainland to east of White Sea was not inundated by Barents or Kara ice sheet during Late Weichselian.
Notes:

Boreas. Vol. 28(1) :234-242 (1999).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.79 -- Quaternary.
519.673 -- Modelling.
.000(410) -- British author.
E7 -- Glaciology: glacial geology and ice ages.
(*501) -- Russia (Federation).
(*685) -- Kara Sea.
(*686) -- Barents Sea.
SPRI record no.: 150065

MARCXML

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001 SPRI-150065
005 20221001170316.0
007 ta
008 221001s1999####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-150065
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aSvendsen, John Inge.
245 10 ‡aMaximum extent of the Eurasian ice sheets in the Barents and Kara Sea region during the Weichselian /‡cJohn Inge Svendsen, and 13 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1999.
300 ## ‡ap. 234-242 :‡bdiag., map.
500 ## ‡aBoreas. Vol. 28(1) :234-242 (1999).
520 3# ‡aPresents preliminary reconstruction of maximum ice-sheet extent during Early/Middle Weichselian (before 50,000 yr BP) and during Late Weichselian (about 20,000-18,000 yr BP). States Early/Middle Weichselian ice sheets were much larger than those of Late Weichselian glacial maximum, concluding that Grosswald's theory is incorrect in depicting ice sheets that are much too large. Theory given by authors allows for half size of Grosswald's reconstruction of ice-sheet extent in Eurasian Arctic in Late Weichselian. Concludes Russian mainland to east of White Sea was not inundated by Barents or Kara ice sheet during Late Weichselian.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.79 -- Quaternary.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a.000(410) -- British author.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*501) -- Russia (Federation).‡2udc
651 #7 ‡a(*685) -- Kara Sea.‡2udc
651 #7 ‡a(*686) -- Barents Sea.‡2udc
773 0# ‡7nnas ‡tBoreas. ‡gVol. 28(1) (1999) ‡wSPRI-56035
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221001