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Morphometric parameters and neotectorphometric parameters and neotectonics of Kalyani River basin, Ganga Plain; a remote sensing and GIS approach
Morphometric parameters and neotectorphometric parameters and neotectonics of Kalyani River basin, Ganga Plain; a remote sensing and GIS approach
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Morphometric parameters and neotectorphometric parameters and neotectonics of Kalyani River basin, Ganga Plain; a remote sensing and GIS approach
Morphometric parameters and neotectorphometric parameters and neotectonics of Kalyani River basin, Ganga Plain; a remote sensing and GIS approach

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Morphometric parameters and neotectorphometric parameters and neotectonics of Kalyani River basin, Ganga Plain; a remote sensing and GIS approach
Morphometric parameters and neotectorphometric parameters and neotectonics of Kalyani River basin, Ganga Plain; a remote sensing and GIS approach
Journal Article

Morphometric parameters and neotectorphometric parameters and neotectonics of Kalyani River basin, Ganga Plain; a remote sensing and GIS approach

2018
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Overview
The drainage basin of the Kalyani river, a tributary of Gomati river has been mapped and delineated using Survey of India toposheets (1:50,000 scale) and remote sensing satellite data. The digitization, slope map preparation and statistical calculations have been carried out with the help of geographical information system (Arc GIS 10). Kalyani a fifth order river exhibits meandering behavior having 2.45 sinuosity index (SI). The Kalyani river basin has about 1235 km2area with NW-SE sloping trend. The total number of first, second, third, and fourth order streams are 373, 71, 12 and 2 respectively, showing dominance of first order streams in the basin. The mean bifurcation ratio (Rb) of the entire basin is 4.8, which indicates that the drainage is not much influenced by geological structures and exhibits dendritic drainage pattern. Relief ratio (Rr) indicates low to medium surface run-off, and low stream power for erosion. The analysis of river bank height 'r' (escarpment) and longitudinal profile of the river closely reveals neotectonic activity at some locations in the basin. To prepare a comprehensive watershed development and management plan, it is important to understand the topography and drainage characteristics of the region.