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(Article of periodic en Anglais - 2012)

Document title

The highest postglacial shore levels and glacio-isostatic uplift pattern in northern Sweden

Authors(s) and Affiliation(s)

BERGLUND M. (1) ;
(1) Dept. of Natural Sciences, Engineering and mathematics, Mid Sweden Univ., Härnösand, SUEDE

Abstract

The detailed clay varve chronology and an extensive knowledge of the highest postglacial shore level elevation (HS) in northern Sweden, along the Bothnian western coast, provides opportunities for determining the pattern of isostatic rise and centre of uplift from the early Holocene. Wave erosion marks in the studied area are seen to be more consistent indicators of HS than glaciofluvial delta levels. The regional 10 ka shore level pattern shows considerable irregularity compared to the current uplift. Central Sweden and western Finland show 10 ka gradients that indicate isostatic response to late (13-10 ka bp) glacial unloading. Indications of a secondary uplift centre west of the present investigation area are reported in previous work; this also suggests rapid isostatic response to unloading. Finally, the possibility of identifying errors in the varve-dated deglaciation chronology via the 10 ka shore level pattern is illustrated

Source

Article of periodic

published at : Geografiska annaler. Series A. Physical geography / ISSN 0435-3676 / CODEN GAPGAP

Editor : Svenska sällskapet för antropologi och geografi, Stockholm - SUEDE (1965)

Millesime : 2012, vol. 94, no3 [pp. 321-337]

Bibliographic references : 3 p.

Collation : 6 fig., 1 tabl.

Language

Anglais

INIST-CNRS, Cote INIST : 2704 A

Digital Object Identifier

Go to electronic document thanks to its DOI : doi:10.1111/j.1468-0459.2011.00443.x

Tous droits réservés © Prodig - Bibliographie Géographique Internationale (BGI), 2013
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