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Record #200851:

Morphodynamic evolution of Kongsfjorden, Svalbard, during the Late Weichselian and Holocene / S.E. Maclachlan, J.A. Howe, M.E. Vardy.

Title: Morphodynamic evolution of Kongsfjorden, Svalbard, during the Late Weichselian and Holocene / S.E. Maclachlan, J.A. Howe, M.E. Vardy.
Author(s): Maclachlan, S. E.
Howe, J. A.
Vardy, M. E.
Date: 2010.
Publisher: London: Geological Society
In: Fjord systems and archives. (2010.),
Abstract: Presents combination of fjord bathymetry and shallow seismic data from Kongsfjorden and Krossfjorden, Svalbard, to characterise and analyse change in fjord coastal environment physiography and glaciosedimentary processes since Last Glacial Maximum. Swath bathymetry reveals that series of several styles of landform, frequently imposed upon each other, permitting reconstruction of relative timings of deposition of each landform with oldest successively overlain and cross-cut by younger landforms and erosional processes.
Notes:

In: Fjord systems and archives / J.A. Howe, and 3 others.

Keywords: 550.384 -- Palaeomagnetism.
551.33 -- Glacial geology.
551.4 -- Geomorphology.
551.462 -- Submarine topography, bottom forms.
551.468.2 -- Fjords, oceanography.
551.794 -- Holocene.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*32) -- Svalbard.
SPRI record no.: 200851

MARCXML

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001 SPRI-200851
005 20220929124003.0
007 ta
008 220929s2010####enkab##|#####|0||#0#eng#d
035 ## ‡aSPRI-200851
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aMaclachlan, S. E.
245 10 ‡aMorphodynamic evolution of Kongsfjorden, Svalbard, during the Late Weichselian and Holocene /‡cS.E. Maclachlan, J.A. Howe, M.E. Vardy.
260 ## ‡aLondon :‡bGeological Society,‡c2010.
300 ## ‡ap. 195-205 :‡bill., maps (1 col.)
500 ## ‡aIn: Fjord systems and archives / J.A. Howe, and 3 others.
520 3# ‡aPresents combination of fjord bathymetry and shallow seismic data from Kongsfjorden and Krossfjorden, Svalbard, to characterise and analyse change in fjord coastal environment physiography and glaciosedimentary processes since Last Glacial Maximum. Swath bathymetry reveals that series of several styles of landform, frequently imposed upon each other, permitting reconstruction of relative timings of deposition of each landform with oldest successively overlain and cross-cut by younger landforms and erosional processes.
530 ## ‡aAlso issued online ‡uurn:doi:10.1144/SP344.14‡uhttps://dx.doi.org/10.1144/SP344.14
650 07 ‡a550.384 -- Palaeomagnetism.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.4 -- Geomorphology.‡2udc
650 07 ‡a551.462 -- Submarine topography, bottom forms.‡2udc
650 07 ‡a551.468.2 -- Fjords, oceanography.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡aB -- Geology and soil sciences.‡2local
651 #7 ‡a(*3) -- Arctic regions.‡2udc
651 #7 ‡a(*32) -- Svalbard.‡2udc
700 1# ‡aHowe, J. A.
700 1# ‡aVardy, M. E.
773 0# ‡7p1am ‡aHowe, J. A. ‡tFjord systems and archives. ‡dLondon : Geological Society, 2010. ‡wSPRI-199569
916 ## ‡a2012/12/20 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220929 ‡bJW