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Geomorphologische Analyse der Tektonik mit RS und GIS Markanda River35,90 €![Hydro-Geomorphological Study of Watershed Using RS and GIS Approach]( "Hydro-Geomorphological Study of Watershed Using RS and GIS Approach")
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Analisi geomorfica della tettonica mediante RS e GIS Fiume Markanda23,99 €![Análise geomórfica da tectónica usando RS e GIS Rio Markanda]( "Análise geomórfica da tectónica usando RS e GIS Rio Markanda")
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Analyse géomorphologique de la tectonique à l'aide de la RS et du SIG Rivière Markanda23,99 €
The Himalayan orogenic belt, formed as a result of collision tectonic processes, shows abundant evidence of neotectonic activity, active tectonics, and the occurrence of historical earthquakes. Its frontal deformation zone is characterized, in some segments, by intermountain longitudinal valleys (duns). Such frontal segments of the Himalaya are marked by the occurrence of multiple mountain fronts.(Kothyari, G., 2010; Lee, C. S L, 2010). The main objective is to carry out topographic analysis using DEM data and calculation of geomorphic indices to decipher tectonic deformation, to prepare a geomorphic map of the study area and analysis of surface processes using remote sensing data, Mapping of channel planform parameters such as longitudinal profile, hypsometry, stream gradient index and analysis of river processes in response to tectonic deformation and finally to integrate all the data to model geomorphic response of the Markanda River basin to tectonic deformation.