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Record #161815:

Glacial deposits and ice-sheet dynamics in the north-central Baltic Sea during the last deglaciation / Riko Noormets, Tom Flodén.

Title: Glacial deposits and ice-sheet dynamics in the north-central Baltic Sea during the last deglaciation / Riko Noormets, Tom Flodén.
Author(s): Noormets, Riko.
Flodén, Tom.
Date: 2002.
In: Boreas. (2002.), Vol. 31(4) (2002)
Abstract: Uses high resolution continuous seismic-reflection profiling data in investigating morphology of glacial deposits under north-central Baltic Sea. Bedrock topography obviously influenced their structure and distribution, directing glacier flows and subglacial meltwater flows into bedrock depressions. Suggests floating, ice-shelf type of glacier existed in Fårö Deep during deglaciation. Ice -marginal deposition took place along grounding line, and together with local outwash fans probably correlates with ice-marginal deposits in Estonia and Levene moraine in Sweden. Variety of deposits show changes in thickness and dynamics of retreating ice sheet well.
Notes:

Boreas. Vol. 31(4) :362-377 (2002).

Keywords: 551.324 -- Land ice.
551.331.5 -- Glacial erosion and protection. Sub-glacial topography.
551.332 -- Glacial deposition.
551.332.5 -- Glacial landforms.
550.834 -- Seismic survey methods.
E7 -- Glaciology: glacial geology and ice ages.
(*611) -- Baltic Sea.
SPRI record no.: 161815

MARCXML

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100 1# ‡aNoormets, Riko.
245 10 ‡aGlacial deposits and ice-sheet dynamics in the north-central Baltic Sea during the last deglaciation /‡cRiko Noormets, Tom Flodén.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2002.
300 ## ‡ap. 362-377 :‡bdiags., table.
500 ## ‡aBoreas. Vol. 31(4) :362-377 (2002).
520 3# ‡aUses high resolution continuous seismic-reflection profiling data in investigating morphology of glacial deposits under north-central Baltic Sea. Bedrock topography obviously influenced their structure and distribution, directing glacier flows and subglacial meltwater flows into bedrock depressions. Suggests floating, ice-shelf type of glacier existed in Fårö Deep during deglaciation. Ice -marginal deposition took place along grounding line, and together with local outwash fans probably correlates with ice-marginal deposits in Estonia and Levene moraine in Sweden. Variety of deposits show changes in thickness and dynamics of retreating ice sheet well.
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.331.5 -- Glacial erosion and protection. Sub-glacial topography.‡2udc
650 07 ‡a551.332 -- Glacial deposition.‡2udc
650 07 ‡a551.332.5 -- Glacial landforms.‡2udc
650 07 ‡a550.834 -- Seismic survey methods.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*611) -- Baltic Sea.‡2udc
700 1# ‡aFlodén, Tom.
773 0# ‡7nnas ‡tBoreas. ‡gVol. 31(4) (2002) ‡wSPRI-56035
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221003