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.
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Vendeur : BuchWeltWeit Ludwig Meier e.K., Bergisch Gladbach, Allemagne
Taschenbuch. Etat : Neu. This item is printed on demand - it takes 3-4 days longer - Neuware -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. 60 pp. Englisch. N° de réf. du vendeur 9786202052276
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Vendeur : AHA-BUCH GmbH, Einbeck, Allemagne
Taschenbuch. Etat : Neu. nach der Bestellung gedruckt Neuware - Printed after ordering - 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. N° de réf. du vendeur 9786202052276
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Vendeur : Revaluation Books, Exeter, Royaume-Uni
Paperback. Etat : Brand New. 60 pages. 8.66x5.91x0.14 inches. In Stock. N° de réf. du vendeur zk6202052279
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Vendeur : moluna, Greven, Allemagne
Etat : New. Dieser Artikel ist ein Print on Demand Artikel und wird nach Ihrer Bestellung fuer Sie gedruckt. Autor/Autorin: Nair Aravind S.Completed Graduation in 2008 from Uni. of Kerala in Geology,Completed PG in 2010 from National College, Bharathidasam Uni. Trichy in Applied Geology.Completed a Diploma in GeoInformatics in 2010 from Centre for Envirnm. N° de réf. du vendeur 176461751
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Vendeur : buchversandmimpf2000, Emtmannsberg, BAYE, Allemagne
Taschenbuch. Etat : Neu. This item is printed on demand - Print on Demand Titel. Neuware -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.VDM Verlag, Dudweiler Landstraße 99, 66123 Saarbrücken 60 pp. Englisch. N° de réf. du vendeur 9786202052276
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