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Record #104744:
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MARC recordLate Weichselian ice recession in the central Barents Sea / Anders Elverhøi, M. Nyland-Berg, Lars Russwurm, Anders Solheim.
| Title: | Late Weichselian ice recession in the central Barents Sea / Anders Elverhøi, M. Nyland-Berg, Lars Russwurm, Anders Solheim. |
| Author(s): | Elverhøi, Anders. Nyland-Berg, M. Russwurm, Lars. Solheim, Anders. |
| Date: | 1990. |
| Publisher: | Dordrecht: Kluwer Academic |
| In: | Geological history of the polar oceans : Arctic versus Antarctic. (1990.), |
| Abstract: | Recent observations of glacial flutes in central Barents Sea represents first direct evidence of existence of grounded ice in this region: glacial flutes suggest ice recession by calving without surge. Ice-marginal features, till ridges and glaciomarine deposits are concentrated in two distinct water depths along present-day 300 and 150 m contour, suggesting halt of 500 to 1000 years in ice recession at each level. Due to lack of sufficient amounts of datable materials in glacigenic sediments, timing of recession can only be discussed in relative terms. |
| Notes: | In: Geological history of the polar oceans : Arctic versus Antarctic / Ulrich Bleil, Jörn Thiede, eds. |
| Keywords: | 551.336 -- Ice ages. 551.79 -- Quaternary. 551.33 -- Glacial geology. 551.332.53 -- Moraines, ground and glacial flutes. 551.332.212 -- Till or boulder clay. 551.332.25 -- Glacio-marine deposits. 551.332.51 -- Ice-marginal landforms. E7 -- Glaciology: glacial geology and ice ages. (*60) -- Arctic Ocean and adjacent waters. (*686) -- Barents Sea. |
| SPRI record no.: | 104744 |
LDR 01986naa#a2200000#a#4500 001 SPRI-104744 005 20231208163309.0 007 ta 008 231208s1990####ne#ab##|#####|0||#0#eng#d 035 ## ‡aSPRI-104744 040 ## ‡aUkCU-P‡beng‡eaacr 245 00 ‡aLate Weichselian ice recession in the central Barents Sea /‡cAnders Elverhøi, M. Nyland-Berg, Lars Russwurm, Anders Solheim. 260 ## ‡aDordrecht :‡bKluwer Academic,‡c1990. 300 ## ‡ap. 289-307 :‡bill., diags., table, maps. 490 0# ‡aNATO ASI Series. Series C, Mathematical and Physical Sciences ;‡v308 500 ## ‡aIn: Geological history of the polar oceans : Arctic versus Antarctic / Ulrich Bleil, Jörn Thiede, eds. 520 3# ‡aRecent observations of glacial flutes in central Barents Sea represents first direct evidence of existence of grounded ice in this region: glacial flutes suggest ice recession by calving without surge. Ice-marginal features, till ridges and glaciomarine deposits are concentrated in two distinct water depths along present-day 300 and 150 m contour, suggesting halt of 500 to 1000 years in ice recession at each level. Due to lack of sufficient amounts of datable materials in glacigenic sediments, timing of recession can only be discussed in relative terms. 650 07 ‡a551.336 -- Ice ages.‡2udc 650 07 ‡a551.79 -- Quaternary.‡2udc 650 07 ‡a551.33 -- Glacial geology.‡2udc 650 07 ‡a551.332.53 -- Moraines, ground and glacial flutes.‡2udc 650 07 ‡a551.332.212 -- Till or boulder clay.‡2udc 650 07 ‡a551.332.25 -- Glacio-marine deposits.‡2udc 650 07 ‡a551.332.51 -- Ice-marginal landforms.‡2udc 650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*686) -- Barents Sea.‡2udc 700 1# ‡aElverhøi, Anders. 700 1# ‡aNyland-Berg, M. 700 1# ‡aRusswurm, Lars. 700 1# ‡aSolheim, Anders. 773 0# ‡7nnam ‡aUlrich Bleil, Jörn Thiede, eds. ‡tGeological history of the polar oceans : Arctic versus Antarctic. ‡dDordrecht : Kluwer Academic, 1990. ‡wSPRI-104236 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231208