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List of Accepted Contributions - GM2.7 To what extent is landscape evolution governed by inherited structures?
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EGU2008-A-00003 Timár, G.; Pišút, P. Changes of the sinuosity of the Morava River (western Slovakia) and their neotectonic origin |
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EGU2008-A-01399 Carter, A How well do we understand the role of ancient sutures in landscape development? An example from Thailand. |
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EGU2008-A-01896 Gunnell, Y.; Harbor, D. Structural underprint, tectonic overprint and drainage integration — do escarpments at passive margins persist or reform? |
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EGU2008-A-05057 Gallagher, K.; Stephenson, J.; Leighton, C. Quantifying differential erosion across ancient structures using 3D Bayesian Partition Modelling |
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EGU2008-A-05631 Bata, T.; Székely, B.; Karátson, D. Determination of morphometric parameters of scoria cones in San Francisco Volcanic Field (USA, Arizona) |
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EGU2008-A-07036 Densmore, A.; Hetzel, R.; Krugh, W.; Seward, D.; Ivy-Ochs, S. The role of tectonic inheritance in simple sediment routing systems |
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EGU2008-A-07173 Bermúdez-Cella, M.; van der Beek, P.; Bernet, M. Fission-track thermochronological evidence for km-scale vertical offsets across the Boconó strike-slip fault, central Venezuelan Andes |
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EGU2008-A-07379 Walcott, R. C.; Summerfield, M. A. Quantifying the effects of spatially variable lithology and uplift rates on landscape morphology (withdrawn) |
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EGU2008-A-07417 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. |
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EGU2008-A-07696 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 |
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EGU2008-A-11358 Wilson, R.; Japsen, P.; Peulvast, J-P.; Bonow, J.; McCaffrey, K.; Chalmers, J.; Green, P. Structure and geomorphology of Mesozoic and Cenozoic landscapes of South Greenland: uplift, erosion and basement reactivation |
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EGU2008-A-11566 Székely, B.; Molnár, G. Do the post-Miocene volcanic features really mark a single paleoaltitude in the Transdanubian Range (Pannonian basin)? |
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EGU2008-A-11781 Reinhardt, L; Ellis, M The primacy of process over structure in landform evolution (withdrawn) |
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EGU2008-A-11855 Ventura, B.; Lisker, F. Tectonic control on long-term landscape development: the example of the Elbe Zone in the northern Bohemian Massif (Germany) |
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