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Record #187030:

An overview of postglacial sediment records from colluvial accumulations in northwestern and north Iceland / Armelle Decaulne, Thorsteinn Saemundsson, Helgi Páll Jónsson.

Title: An overview of postglacial sediment records from colluvial accumulations in northwestern and north Iceland / Armelle Decaulne, Thorsteinn Saemundsson, Helgi Páll Jónsson.
Author(s): Decaulne, Armelle.
Saemundsson, Thorsteinn.
Jónsson, Helgi Páll.
Date: 2009.
In: Arctic, Antarctic, and Alpine Research. (2009.), Vol. 41(1) (2009)
Abstract: Describes active denudation processes occurring on slopes in northern and north-western Iceland contributing to build-up of large colluvial cones. Vertical sections in colluvial cones exhibit characteristic stratigraphy with successions of material from mass-movements interbedded with soil horizons occurring throughout Holocene, under periglacial conditions of varying intensity. Alternating organic and minerogenic units are indicators of phases of slope activity and stability.
Notes:

Arctic, Antarctic, and Alpine Research. Vol. 41(1) :37-47 (2009).

Keywords: 551.1/.4 -- Geology.
551.3.051 -- Sedimentation and stratification.
551.3.053 -- Geological erosion, corrosion and disintegration.
551.33 -- Glacial geology.
551.4 -- Geomorphology.
551.7 -- Stratigraphy.
551.794 -- Holocene.
B -- Geology and soil sciences.
(*3) -- Arctic regions.
(*35) -- Iceland.
SPRI record no.: 187030

MARCXML

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100 1# ‡aDecaulne, Armelle.
245 13 ‡aAn overview of postglacial sediment records from colluvial accumulations in northwestern and north Iceland /‡cArmelle Decaulne, Thorsteinn Saemundsson, Helgi Páll Jónsson.
260 ## ‡a[S.l.] :‡b[s.n.],‡c2009.
300 ## ‡ap. 37-47 :‡bill., diags., maps.
500 ## ‡aArctic, Antarctic, and Alpine Research. Vol. 41(1) :37-47 (2009).
520 3# ‡aDescribes active denudation processes occurring on slopes in northern and north-western Iceland contributing to build-up of large colluvial cones. Vertical sections in colluvial cones exhibit characteristic stratigraphy with successions of material from mass-movements interbedded with soil horizons occurring throughout Holocene, under periglacial conditions of varying intensity. Alternating organic and minerogenic units are indicators of phases of slope activity and stability.
530 ## ‡aAlso issued online ‡uurn:doi:10.1657/1938-4246(08-037)[DECAULNE]2.0.CO;2‡uhttps://dx.doi.org/10.1657/1938-4246(08-037)[DECAULNE]2.0.CO;2
650 07 ‡a551.1/.4 -- Geology.‡2udc
650 07 ‡a551.3.051 -- Sedimentation and stratification.‡2udc
650 07 ‡a551.3.053 -- Geological erosion, corrosion and disintegration.‡2udc
650 07 ‡a551.33 -- Glacial geology.‡2udc
650 07 ‡a551.4 -- Geomorphology.‡2udc
650 07 ‡a551.7 -- Stratigraphy.‡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(*35) -- Iceland.‡2udc
700 1# ‡aSaemundsson, Thorsteinn.
700 1# ‡aJónsson, Helgi Páll.
773 0# ‡7nnas ‡tArctic, Antarctic, and Alpine Research. ‡gVol. 41(1) (2009) ‡wSPRI-211524
916 ## ‡a2009/04/09 -- JW
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20221007 ‡bJW