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A major developmental factor, largely neglected, is persistent disturbance of high mountain fluvial systems by many successive landslides.
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Total forest C stocks differed among land units (287 to 478 Mg C ha− 1 in limestone mountains and fluvial terraces, respectively).
Here, we test the application of four medium resolution DEM products (30 m = SRTM, ASTER, AW3D; 12 m = TanDEM-X) for qualitative and quantitative analysis of a fluvial mountain landscape using the Dades River catchment (High Atlas Mountains, Morocco).
General and specific approaches on the study of flood hazards are considered for three fluvial environments: mountain streams, alluvial fans, and alluvial rivers.
North-facing fault scarps on mountain slopes and the fluvial terraces observed along the fault, suggesting that vertical displacement is down on the north (Nakata 1982).
Sediments were transported to the basin from uplifting Carpathian and Dinaric mountains, with particularly deep fluvial sediments being deposited in the Pleistocene during the uplift of the Transdanubian Mountains.
Sediments were transported to the basin from the uplifting Carpathian and Dinaric mountains, with particularly deep fluvial sediments being deposited in the Pleistocene epoch during the Transdanubian Mountains' formation.
Erosion by glacial and fluvial processes shapes mountain landscapes in a long-recognized and characteristic way.
Mixed bedrock alluvial rivers bedrock channels lined with a discontinuous alluvial cover are key agents in the shaping of mountain belt topography by bedrock fluvial incision.
We present a novel regional approach to automatically differentiate between fluvial and glacial mountain landscapes based on the relation of multi-scale curvature and drainage area.
Neotectonics is a major factor controlling landform development in tectonically active regions, and it has significantly affected fluvial systems and mountain-front landscapes in the Sarvestan area of the central Zagros, Iran.
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