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- > Weathering - erosion - sedimentation. New studies in morphodynamics and processes (supprimer)
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Par Collection Par Auteur- PFEFFER, K.-H., (Editeur scientifique) (3)
- KHADKIKAR, A.S. (1)
- MALIK, J.N. (1)
- VELDKAMP, A. (1)
- XILIN LIU (1)
- 1996 (3)
- Africa ; Base level ; Cenozoic ; Concept ; Eastern Africa ; Fluvial dynamics ; Geomorphogenesis ; Planation ; Rift ; Tectonics ; Vertical movement (1)
- Afrique ; Afrique de l'Est ; Aplanissement ; Concept ; Cénozoïque ; Dynamique fluviale ; Géomorphogenèse ; Mouvement vertical ; Niveau de base ; Rift ; Tectonique (1)
- Alluvial cone ; China ; Debris flow ; Geomorphometry ; Guangxi Zhuang ; Mass movement ; Model ; Sedimentology ; Slope ; Slope gradient ; Statistics (1)
- Bassin-versant ; Crue ; Fluviatile ; Géométrie hydraulique ; Inde ; Mahārāshtra ; Paléohydrologie ; Pédogenèse ; Remplissage sédimentaire ; Structure sédimentaire (1)
- Channel geometry ; Flood ; Fluvial processes ; India ; Maharashtra ; Palaeohydrology ; Pedogenesis ; Sediment filling ; Sedimentary structure ; Watershed (1)
- Chine ; Coulée boueuse ; Cône de déjection ; Guangxi ; Géomorphométrie ; Modèle ; Mouvement de masse ; Pente de versant ; Statistique ; Sédimentologie ; Versant (1)
- Weathering - erosion - sedimentation. New studies in morphodynamics and processes (3)
- Morphologic characteristics of debris flow fans in Xiaojiang Valley of southwestern China (1)
- Palaeoflood analysis of channel-fill deposits, central Tapti river basin, India (1)
- late Cenozoic landform development in East Africa: the role of near base level planation within the dynamic etchplanation concept (1)
- late Cenozoic landform development in East Africa: the role of near base level planation within the dynamic etchplanation concept
- near base level. It is therefore proposed to elaborate the etchplanation concept with fluvial dynamics. Late Cenozoic planation events in East Africa were triggered by a major base level rise due to the combined effects of eustatic sea level rise
- The Quaternary sediments exposed on the banks of the river Aner which is a tributary of the river Tapti, near Piloda (district Dhule), western India, reveal 3 channel-fill structures, spatially at the same level. The AA. therefore present here
- of depositional processes on the morphologic characteristics of debris flow fans is studied through depositional model experiments. These experiments were conducted near a debris flow gully just after debris flows took place.