Deciphering a non-glacial/glacial landscape mosaic in the northern Swedish mountains

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Fältnamn	Indikatorer	Metadata
000		04210naa a2200421 4500
001		oai:DiVA.org:su-19944
003		SwePub
008		090101s2008 \| \|\|\|\|\|\|\|\|\|\|\|000 \|\|eng\|
024	7	a https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-199442 URI
024	7	a https://doi.org/10.1016/j.geomorph.2007.02.0182 DOI
040		a (SwePub)su
041		a engb eng
042		9 SwePub
072	7	a ref2 swepub-contenttype
072	7	a art2 swepub-publicationtype
100	1	a Goodfellow, Bradleyu Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK),paleoglaciologi/paleoglaciology4 aut0 (Swepub:su)bgood
245	1 0	a Deciphering a non-glacial/glacial landscape mosaic in the northern Swedish mountains
264	1	b Elsevier BV,c 2008
338		a print2 rdacarrier
500		a Financial support was provided by the Swedish Society for Anthropology and Geography (SSAG) Andreéfonden, Axel Lagrelius' fund, and Swedish Research Council grants 621-2001-2331 and 621-2005-4972.
520		a Relict surfaces contain information on past surface processes and long-term landscape evolution. A detailed investigation of relict non-glacial surfaces in a formerly glaciated mountain landscape of northern Sweden was completed, based on interpretation of colour infrared aerial photographs, analysis in a GIS, and fieldwork. Working backwards from landscape to process, surfaces were classified according to large- and small-scale morphologies that result from the operation of non-glacial processes, the degree of weathering, regolith characteristics, and the style of glacial modification. Surfaces were also compared in the GIS according to elevation, slope angle, and bedrock lithology. The study revealed five types of relict non-glacial surfaces but also two types of extensively weathered glacial surfaces that were transitional to relict non-glacial surfaces, illustrating spatially variable processes and rates of non-glacial and glacial landscape evolution. Rather than being static preglacial remnants, relict non-glacial surfaces are dynamic features that have continued to evolve during the Quaternary. The classification provides hypotheses for landscape evolution that can be field tested through, for example, terrestrial cosmogenic nuclide studies and geochemical analyses of fine matrix materials. The classification may be applicable to relict non-glacial surfaces in other formerly glaciated landscapes
650	7	a NATURVETENSKAPx Geovetenskap och miljövetenskapx Geologi0 (SwePub)105042 hsv//swe
650	7	a NATURAL SCIENCESx Earth and Related Environmental Sciencesx Geology0 (SwePub)105042 hsv//eng
653		a Relict surface
653		a Glaciation
653		a Landscape evolution
653		a Blockfield
653		a Northern Sweden
653		a GIS
700	1	a Stroeven, Arjenu Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK),paleoglaciologi/paleoglaciology4 aut0 (Swepub:su)stroe
700	1	a Hättestrand, Clasu Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK),paleoglaciologi/paleoglaciology4 aut0 (Swepub:su)classe
700	1	a Kleman, Johanu Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK),paleoglaciologi/paleoglaciology4 aut0 (Swepub:su)kleman
700	1	a Jansson, Kristeru Stockholms universitet,Institutionen för naturgeografi och kvartärgeologi (INK),paleoglaciologi/paleoglaciology4 aut0 (Swepub:su)krister
710	2	a Stockholms universitetb Institutionen för naturgeografi och kvartärgeologi (INK)4 org
773	0	t Geomorphologyd : Elsevier BVg 93:3-4, s. 213-232q 93:3-4<213-232x 0169-555X
856	4	u http://www.sciencedirect.com/science?_ob=ArticleURL&_udi=B6V93-4N7SBGK-1&_user=2195977&_coverDate=01%2F15%2F2008&_rdoc=5&_fmt=summary&_orig=browse&_srch=doc-info(%23toc%235887%232008%23999069996%23673772%23FLA%23display%23Volume)&_cdi=5887&_sort=d&_docanchor=&_ct=25&_acct=C000035218&_version=1&_urlVersion=0&_userid=2195977&md5=7cdde3d4f365d9524e12674e522cb7a4
856	4 8	u https://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-19944
856	4 8	u https://doi.org/10.1016/j.geomorph.2007.02.018

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Av författaren/redakt...: Goodfellow, Brad ...; Stroeven, Arjen; Hättestrand, Cla ...; Kleman, Johan; Jansson, Krister

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