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Oral Programme GM9.1/CR1.70

GM9.1/CR1.70

Cold Region Geomorphology (co-organized)
Convener: M. Spagnolo 
Co-Conveners: I. Gärtner-Roer , S. Lukas 
Session details
Oral Programme
 / Tue, 24 Apr, 08:30–12:00 / Room 21
Poster Programme
 / Attendance Tue, 24 Apr, 17:30–19:00 / Hall XL
Add this session to your personal programme

Tuesday, 24 Apr 2012
Room 21
Chairperson: Matteo Spagnolo
08:30–09:00
EGU2012-3257
Effects of tectonism on glacial and paraglacial processes- a New Zealand case study (solicited)
J. Shulmeister
09:00–09:15
EGU2012-1539
Lithological and fluvial influences on clast shape measurements in a temperate alpine environment: a case study from Fox Glacier, New Zealand
M. Brook and S. Lukas
09:15–09:30
EGU2012-10661
Detrital flux in glacial and peri-glacial domain: the example of the Bossons glacier (Haute Savoie, Mont-Blanc Massif)
C. Godon, J-F. Buoncristiani, and J-L. Mugnier
09:30–09:45
EGU2012-9900
A new assessment of distribution and activity of permafrost landforms in the Tröllaskagi peninsula, northern Iceland
K.S. Lilleøren, I. Gärtner-Roer, and B. Etzelmüller
09:45–10:00
EGU2012-9573
On the relationship between surface flow velocity and climatic conditions at three rock glaciers in central Austria
A. Kellerer-Pirklbauer and V. Kaufmann
COFFEE BREAK
Chairperson: Sven Lukas
10:30–11:00
EGU2012-4699
Bedrock properties and glacial processes and landforms - some principles and examples (solicited)
M. Krabbendam
11:00–11:15
EGU2012-173 | Presentation
Controls on the location and geometry of glacial overdeepening
C. Lloyd, C. Clark, and D. Swift
11:15–11:30
EGU2012-9833
Late-glacial ice dynamics of the northeastern sector of the Cordilleran Ice Sheet reconstructed from the glacial landform record
M. Margold, K.N. Jansson, J. Kleman, and A.P. Stroeven
11:30–11:45
EGU2012-11541
Interglacial geomorphic dynamics during the Quaternary: Does glacial erosion dominates interglacial adjustment?
T. Hoffmann and E.A. Johnson
11:45–12:00
EGU2012-13086
Dissolution of calcite in glacial water; evidence of inhibition and consequences for subglacial speleogenesis.
S.-E. Lauritzen