BORA - UiB

Bergen Open Research Archive

Temporale og romlige sedimentasjonstrender i en distal-glasial innsjø, gjennom Den Lille Istid

Bergen Open Research Archive

Show simple item record

dc.contributor.author Skulstad, Eva Marie
dc.date.accessioned 2012-03-13T09:14:41Z
dc.date.available 2012-03-13T09:14:41Z
dc.date.issued 2011-09-01
dc.date.submitted 2011-09-01 en
dc.identifier.uri http://hdl.handle.net/1956/5703
dc.description.abstract The sedimentation processes in an arctic distal-glacier fed lake Jægervatn (3 m. a.s.l.), located in northern Norway, has been studied by means of core analysis in addition to quaternary mapping of the catchment area of Jægervatn. The cores consist of six HTH - sediment cores (JVS104 - JVS604) and one longer piston core (JVP203), retrieved along a south - north oriented transect in the lake covering 2000 m. The physical properties of the lacustrine sediments have been examined including visual log, X-ray, X-ray fluorescence (XRF), magnetic susceptibility (MS), frequency and temperature susceptibility (χbulk, 293K and 77K), loss on ignition (LOI), water content (WC), dry bulk density (DBD) and grain size distribution. The main focus was to study the temporal and spatial distribution of sediments in Jægervatn and assess to what extent the observed patterns could be related to glacial and extra-glacial activity. Based on result from the laboratory methods a sedimentation model for Jægervatn has been developed. The analysis of the cores have recognized two dominating sedimentary units in Jægervatn; unit B which is dominated by paraglacial processes and unit A which is dominated by glacial activity. Unit B was deposited during the Medial Warm Period" (MWD), whereas Unit A was deposted during the Little Ice Age (LIA). The latter period started in 1490 AD and lasted until 1920AD in the study area, possibly with two separate advances occurring around 1660 AD and 1830 AD, respectively. A third unit is also revealed and has been deposited during marine environments when Jægervatn was connected to fjord settings. The Equilibrium-line-altitude (ELA) lowering during the LIA was 57m, but even so it lead to over a trippeling of the sedimentation rate as recorded in Jægervatn, although the spatial pattern was much the same as during earlier periods. en
dc.format.extent 13133139 bytes en
dc.format.mimetype application/pdf en
dc.language.iso nob en
dc.publisher The University of Bergen en
dc.title Temporale og romlige sedimentasjonstrender i en distal-glasial innsjø, gjennom Den Lille Istid en
dc.type Master thesis en
dc.type.degree Master en
dc.type.course GEO350 en
dc.subject.nsi VDP::Social science: 200::Human geography: 290 en
dc.subject.archivecode Mastergrad en
dc.subject.nus 733111 en
dc.type.program MASV-GEOG en


Files in this item

 

This item appears in the following Collection(s)

Show simple item record

Search BORA


Browse

My Account