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Record #183958:

Late Weichselian deglaciation and sea level history of St Jonsfjorden, Spitsbergen: a contribution to ice sheet reconstruction / David J.A. Evans, Brice R. Rea.

Title: Late Weichselian deglaciation and sea level history of St Jonsfjorden, Spitsbergen: a contribution to ice sheet reconstruction / David J.A. Evans, Brice R. Rea.
Author(s): Evans, David J. A.
Rea, Brice R.
Date: 2005.
In: Scottish Geographical Journal. (2005.), Vol. 121(2) (2005)
Abstract: Presents partial reconstruction of late Weichselian deglaciation of St Jonsfjorden, based upon radiocarbon-dated emerged marine sediments and raised shoreline fragments. Data support previously reported occurrence of two sets of shorelines on west coast of Spirsbergen, older set at 60 m located around fjord mouth and younger set below 46 m. Occurrence in north-west spitsbergen of well preserved extensive shorelines that are demonstrably older than late Weichselian can be explained either by survival beneath cold-based glacier ice, or ice-free conditions throughout glacial cycle.
Notes:

Scottish Geographical Journal. Vol. 121(2) :175-202 (2005).

Keywords: 551.32 -- Glaciology.
551.324 -- Land ice.
551.324.22 -- Glaciers.
551.324.63 -- Land ice, advance and retreat.
551.324.24 -- Ice sheets and caps.
551.35 -- Marine sediments.
551.351 -- Coastal deposits.
551.4 -- Geomorphology.
551.583 -- Climatic changes.
551.461.2 -- Sea level, fluctuations.
551.588.5 -- Climate, relationship with ice.
551.794 -- Holocene.
E7 -- Glaciology: glacial geology and ice ages.
(*3) -- Arctic regions.
(*32) -- Svalbard.
(*324) -- Spitsbergen.
SPRI record no.: 183958

MARCXML

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100 1# ‡aEvans, David J. A.
245 10 ‡aLate Weichselian deglaciation and sea level history of St Jonsfjorden, Spitsbergen :‡ba contribution to ice sheet reconstruction /‡cDavid J.A. Evans, Brice R. Rea.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2005.
300 ## ‡ap. 175-202 :‡bill., diags., tables, maps.
500 ## ‡aScottish Geographical Journal. Vol. 121(2) :175-202 (2005).
520 3# ‡aPresents partial reconstruction of late Weichselian deglaciation of St Jonsfjorden, based upon radiocarbon-dated emerged marine sediments and raised shoreline fragments. Data support previously reported occurrence of two sets of shorelines on west coast of Spirsbergen, older set at 60 m located around fjord mouth and younger set below 46 m. Occurrence in north-west spitsbergen of well preserved extensive shorelines that are demonstrably older than late Weichselian can be explained either by survival beneath cold-based glacier ice, or ice-free conditions throughout glacial cycle.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.22 -- Glaciers.‡2udc
650 07 ‡a551.324.63 -- Land ice, advance and retreat.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc
650 07 ‡a551.35 -- Marine sediments.‡2udc
650 07 ‡a551.351 -- Coastal deposits.‡2udc
650 07 ‡a551.4 -- Geomorphology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.461.2 -- Sea level, fluctuations.‡2udc
650 07 ‡a551.588.5 -- Climate, relationship with ice.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡aE7 -- Glaciology: glacial geology and ice ages.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*32) -- Svalbard.‡2udc
651 #7 ‡a(*324) -- Spitsbergen.‡2udc
700 1# ‡aRea, Brice R.
773 0# ‡7nnas ‡tScottish Geographical Journal. ‡gVol. 121(2) (2005) ‡wSPRI-150833
916 ## ‡a2008/08/29 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220929 ‡bJW