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This hypothesis has been tested by applying two geomorphic indices, the Stream-gradient index (SL) and the Valley width/height ratio (Vf), as well as by considering surface and subsoil information about the sedimentary infill of the Ametler graben.
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On the basis of the presence of characteristic geomorphic features, the study area is divided into two geomorphic units: fluvial deltaic plain (FDP) and fluvio-tidal deltaic plain (FTDP).
Three geomorphic indices (hypsometry, river long profile analysis and stream-length gradient index) are applied to freely available DEM data in order to develop the qualitative and quantitative (relative to study area) understanding of how the hillslope and river systems respond to the effects of tectonic activity and climate change.
On the basis of terrace correlation between seventeen geomorphic sections, multiwave headward erosion initiated by the Yellow River along this gorge has been reconstructed.
At least three geomorphic surfaces have formed during an interval from the middle Pleistocene to the Holocene.
Soil samples collected from three geomorphic surfaces were scanned in the visible and near infrared spectral range.
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