SwePub
Sök i SwePub databas

  Extended search

Träfflista för sökning "(WFRF:(Höpfner M.)) pers:(Höpfner M.) lar1:(cth) pers:(Strong K.) pers:(Taylor J) pers:(Notholt J.) "

Search: (WFRF:(Höpfner M.)) pers:(Höpfner M.) lar1:(cth) pers:(Strong K.) pers:(Taylor J) pers:(Notholt J.)

  • Result 1-2 of 2
Sort/group result
   
EnumerationReferenceCoverFind
1.
  •  
2.
  • Stroeven, Arjen, 1963-, et al. (author)
  • Erosional landscapes
  • 2013
  • In: <em>Treatise on Geomorphology</em>. - San Diego : Academic Press. - 9780123747396 ; , s. 100-112
  • Book chapter (peer-reviewed)abstract
    • Glacial erosion has created distinctive types of landscapes reflecting the extent, duration, and processes of the parent glaciers. Alpine landscapes are representative of pervasive erosion at the local scale. Landscapes formerly covered by larger scale glaciations display a wide range of appearances, from intensively eroded to preserved. Landscapes of selective linear erosion were formed, where subglacial melting occurred along certain corridors that were flanking regions of subglacial freezing. Landscapes of areal scouring were formed where subglacial melting on low-relief surfaces allowed spatially extensive subglacial stripping to dominate. Landscapes of little or no erosion indicate a dominance of subglacial freezing conditions.
  •  
Skapa referenser, mejla, bekava och länka
  • Result 1-2 of 2
Type of publication
conference paper (1)
book chapter (1)
Type of content
peer-reviewed (2)
Author/Editor
Barker-Ruchti, Natal ... (1)
Kerr, Roslyn (1)
Heyman, Jakob (1)
Harbor, Jonathan (1)
Stroeven, Arjen, 196 ... (1)
Moreham, Robert (1)
University
Stockholm University (1)
Örebro University (1)
Language
English (2)
Research subject (UKÄ/SCB)
Natural sciences (2)
Engineering and Technology (1)
Year

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