EGU General Assembly 2008
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  Oral Programme - GM2.7 To what extent is landscape evolution governed by inherited structures?

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Convener: Carter, A.
Co-Convener: Gallagher, K., Brown, R.

Wednesday, 16 April 2008

Lecture Room: Lecture Room 18

Chairperson: N.N.

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8:30 - 8:45
EGU2008-A-01896;  GM2.7-1WE1O-001
Gunnell, Y.; Harbor, D.
Structural underprint, tectonic overprint and drainage integration do escarpments at passive margins persist or reform? (solicited)

8:45 - 9:00
EGU2008-A-07417;  GM2.7-1WE1O-002
Redfield, T. F.; Osmundsen, P. T.
The Tjellefonna fault system of north Western Norway: linking late-Caledonian extension, post-Caledonian normal faulting, and Tertiary rock column uplift with the great landslide/tsunami event of 1756.

9:00 - 9:15
EGU2008-A-11855;  GM2.7-1WE1O-003
Ventura, B.; Lisker, F.
Tectonic control on long-term landscape development: the example of the Elbe Zone in the northern Bohemian Massif (Germany)

9:15 - 9:30
EGU2008-A-07036;  GM2.7-1WE1O-004
Densmore, A.; Hetzel, R.; Krugh, W.; Seward, D.; Ivy-Ochs, S.
The role of tectonic inheritance in simple sediment routing systems (solicited)

9:30 - 9:45
EGU2008-A-07696;  GM2.7-1WE1O-005
Landgraf, A. ; Zielke, O.; Arrowsmith, R.; Ballato, P.; Strecker, M.; Friedrich, A.
Can numerical fault-slip modeling help differentiate simple landscapes from composite landscapes that have been affected by changes in tectonic conditions? Insights from the south-central Alborz mountains, Iran

9:45 - 10:00
EGU2008-A-05057;  GM2.7-1WE1O-006
Gallagher, K.; Stephenson, J.; Leighton, C.
Quantifying differential erosion across ancient structures using 3D Bayesian Partition Modelling


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