Change search
ReferencesLink to record
Permanent link

Direct link
Chronology and dynamics of the Yukon sector of the northern Cordilleran ice sheet
Stockholm University, Faculty of Science, Department of Physical Geography and Quaternary Geology. (paleoglaciologi/paleoglaciology)
Stockholm University, Faculty of Science, Department of Physical Geography and Quaternary Geology. (paleoglaciologi/paleoglaciology)
2007 (English)In: Quaternary International, 2007Conference paper (Refereed)
Abstract [en]

The history of the Cordilleran ice sheet (CIS) of western North Amer¬ica is relatively poorly understood despite over one hundred years of field studies. In contrast to other ice sheets, except for the West Antarc¬tic ice sheet, the CIS was largely resting on mountainous terrain. Due to its physiographic characteristics, of having been fed by confluent flow from both the Coast Range and the Rocky Mountains, it appears to have been one of the most dynamic ice age features on Earth. There is a reasonably good understanding of the timing of maximum glacia¬tion for the last glacial cycle (LGM) and for the almost instantaneous onset of postglacial conditions, based on radiocarbon dates. This gen¬eralized picture is better-documented for the southern than for the northern CIS. We focus on the succession of flow patterns of the CIS by mapping glacial lineation systems and ribbed moraine. These land¬forms define the spatial flow organisation, and give insight into the subglacial thermal regime. In addition to the dominating Late Wiscon¬sinan flow pattern, we discovered numerous fragments of older, over¬ridden and partially destroyed lineation systems. These shed light on older, albeit undated, ice sheet configurations with more easterly ice divide locations than during the late Wisconsinan ice sheet configura¬tion. Mapping in the Pelly Mountains region, Yukon Territory, shows remnant relict glacial lineation systems, relict upland surfaces, well-defined end- and lateral moraine systems and abundant LGM lineation systems in the major glacial troughs. We test the hypothesis that sub¬glacial preservation of relict lineation systems and relict uplands define the subglacial temperature distribution of subsequent ice sheets (i.e LGM), particularly the potential occurrence of frozen bed conditions. We will present cosmogenic 10Be ages on end- and lateral moraines that define the upper/distal limit of the CIS in this region, to test wheth¬er mountain summits were likely overridden (and preserved beneath cold-based ice) or were in effect nunataks during maximum of glacia¬tion. A preliminary study of fabric of two superimposed till sheets ex¬posed in a section along the Nisutin River, in an area inferred to have relict lineation systems, showed consistency with inferred ice flow di¬rections from satellite imagery. The presence of a till sheet above the till sheet which, based on till fabric analysis, forms the relict lineations in the area, potentially shows that preservation may have been under influence of slow-flowing ice rather than (just) cold-based conditions.

Place, publisher, year, edition, pages
URN: urn:nbn:se:su:diva-16815OAI: diva2:183335
Available from: 2007-12-06 Created: 2007-12-06Bibliographically approved

Open Access in DiVA

No full text

Other links

Search in DiVA

By author/editor
Stroeven, ArjenKleman, Johan
By organisation
Department of Physical Geography and Quaternary Geology

Search outside of DiVA

GoogleGoogle Scholar
The number of downloads is the sum of all downloads of full texts. It may include eg previous versions that are now no longer available

Total: 24 hits
ReferencesLink to record
Permanent link

Direct link