EGU - European Geosciences Union second General Assembly 2005, Vienna,
Austria, 24 - 29 April 2005
GEOQUEBEC,
24-27 October Octobre 2004, Québec, 57th CANADIAN GEOTECHNICAL
CONFERENCE
The
Geological Society of London William Smith Meeting, 4th & 5th October
2004 - Burlington House, London: Earths Dynamic Surface
Catastrophe and Continuity In Landscape Evolution.
NH3.11 Terrain analysis using DTM and landslides (co-listed in GM)
Convener: Jaboyedoff, M. and Co-Convener: Couture, R.; Derron,
M.
EGU
- 1st General Assembly Nice, France, 25 - 30 April 2004
NH3.07
Terrain analysis using DTM and landslides
Convener:
Jaboyedoff, M. and Co-Convener(s): Couture, R.
Terrain
analysis is one of the new challenges of the hazard assessment, knowing
the rapid increase in availability and in precision of DTM. Geology
plays a great role on geomorphology, a fine analysis of DTM permits
to outline the structure and geology of a poorly known region and also
to systematically analyze known regions. Several landslide and erosion
areas can be detected by simple or more sophisticated DTM analysis.
Modelling of landslides and erosion processes are dependent on the DTM
quality. This is a basic challenge for the future research of erosion
processes study and hazard assessment.
NH3.08
Modelling landslides as part of erosive processes
Convener:
Jaboyedoff, M. and Co-Convener(s): Couture, R.
Landslides are part of the erosion processes. Quantification of erosion
is important, because its understanding as part of geodynamics has a
great importance for hazard assessment. The relationships of particular
geodynamic contexts give information on the velocity of the erosive
processes. Thus the questions are: where are located preferentially
the landslides? And what are the importance of the mass flux ratio down
to the sea level (or below) of the landslides versus others erosive
processes.