SwePub
Sök i LIBRIS databas

  Extended search

WFRF:(Kent David M.)
 

Search: WFRF:(Kent David M.) > (2010-2014) > SOUTHERN LAURENTIDE...

SOUTHERN LAURENTIDE ICE SHEET DEAD-ICE TOPOGRAPHY: THE ‘WISCONSIN VIEW' AND NEW OPPORTUNITIES

Johnson, Mark D., 1954 (author)
Gothenburg University,Göteborgs universitet,Institutionen för geovetenskaper,Department of Earth Sciences
Mickelson, David M. (author)
Clayton, Lee (author)
show more...
Attig, John W. (author)
Ham, Nelson R. (author)
Syverson, Kent M. (author)
show less...
 (creator_code:org_t)
2011
2011
English.
In: Geological Society of America abstracts with programs Minneapolis 2011.
  • Conference paper (peer-reviewed)
Abstract Subject headings
Close  
  • Much of the Late Glacial Maximum margin of the Laurentide Ice Sheet in Wisconsin is marked by extensive tracts of dead-ice topography. These areas are characterized by numerous irregular hummocks and swales occurring together in a band parallel to the former ice-margin position and extending several kilometers up ice. Ice-walled-lake plains are a common feature in these landscapes. We have analyzed the geomorphology and internal composition of these hummocks while making county maps throughout the state. This dead-ice topography is produced by gradual melting of stagnant ice that had thick supraglacial debris. The supraglacial debris was derived from the ice bed by freezing-on, thrusting, and stacking near the margin. There is abundant evidence that the ice lobes that left behind hummocks topography advanced into permafrosted terrain and, in many cases, likely at fast-flow rates (surging or streaming). These two factors, along with up-gradient bed slopes in places, accentuated the marginal thrusting processes and increased the amount of supraglacial debris. In places, preferred orientation of hummocks likely reflects structures in the parent ice. The presence of tunnel channels cutting through hummocky terrains is also an expression of ice with a frozen toe and rapid ice flow. Following stagnation, the presence of permafrost controlled the rate and timing of dead-ice melting.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Multidisciplinär geovetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geosciences, Multidisciplinary (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences (hsv//eng)

Publication and Content Type

ref (subject category)
kon (subject category)

To the university's database

Find more in SwePub

By the author/editor
Johnson, Mark D. ...
Mickelson, David ...
Clayton, Lee
Attig, John W.
Ham, Nelson R.
Syverson, Kent M ...
About the subject
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
and Geosciences Mult ...
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
and Geology
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
Articles in the publication
By the university
University of Gothenburg

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