SwePub
Sök i LIBRIS databas

  Extended search

id:"swepub:oai:DiVA.org:umu-76279"
 

Search: id:"swepub:oai:DiVA.org:umu-76279" > Lake Floor Morpholo...

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist
  • Vogel, HendrikInstitute of Geological Sciences, University of Bern, Bern, Switzerland (author)

Lake Floor Morphology and Sediment Architecture of Lake Tornetrask, Northern Sweden

  • Article/chapterEnglish2013

Publisher, publication year, extent ...

  • 2016-11-15
  • Wiley-Blackwell,2013
  • printrdacarrier

Numbers

  • LIBRIS-ID:oai:DiVA.org:umu-76279
  • https://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-76279URI
  • https://doi.org/10.1111/geoa.12006DOI

Supplementary language notes

  • Language:English
  • Summary in:English

Part of subdatabase

Classification

  • Subject category:ref swepub-contenttype
  • Subject category:art swepub-publicationtype

Notes

  • Here we present datasets from a hydroacoustic survey in July 2011 at Lake Tornetrask, northern Sweden. Our hydroacoustic data exhibit lake floor morphologies formed by glacial erosion and accumulation processes, insights into lacustrine sediment accumulation since the beginning of deglaciation, and information on seismic activity along the Parvie Fault. Features of glacial scouring with a high-energy relief, steep slopes, and relative reliefs of more than 50m are observed in the large W-basin. The remainder of the lacustrine subsurface appears to host a broad variety of well preserved formations from glacial accumulation related to the last retreat of the Fennoscandian ice sheet. Deposition of glaciolacustrine and lacustrine sediments is focused in areas situated in proximity to major inlets. Sediment accumulation in distal areas of the lake seldom exceeds 2m or is not observable. We assume that lack of sediment deposition in the lake is a result of different factors, including low rates of erosion in the catchment, a previously high lake level leading to deposition of sediments in higher elevated paleodeltas, tributaries carrying low suspension loads as a result of sedimentation in upstream lakes, and an overall low productivity in the lake. A clear off-shore trace of the Parvie Fault could not be detected from our hydroacoustic data. However, an absence of sediment disturbance in close proximity to the presumed fault trace implies minimal seismic activity since deposition of the glaciolacustrine and lacustrine sediments.

Subject headings and genre

Added entries (persons, corporate bodies, meetings, titles ...)

  • Wagner, BerndInstitute of Geology and Mineralogy, University of Cologne, Köln, Germany (author)
  • Rosen, PeterUmeå universitet,Institutionen för ekologi, miljö och geovetenskap(Swepub:umu)pero0001 (author)
  • Institute of Geological Sciences, University of Bern, Bern, SwitzerlandInstitute of Geology and Mineralogy, University of Cologne, Köln, Germany (creator_code:org_t)

Related titles

  • In:Geografiska Annaler. Series A, Physical Geography: Wiley-Blackwell95:2, s. 159-1700435-36761468-0459

Internet link

Find in a library

To the university's database

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Find more in SwePub

By the author/editor
Vogel, Hendrik
Wagner, Bernd
Rosen, Peter
About the subject
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
Articles in the publication
Geografiska Anna ...
By the university
Umeå University

Search outside SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Close

Copy and save the link in order to return to this view