
Atul Kumar
Phone: 9675566994
Address: Department of Geography
N.R.E.C. College Khurja, Bulandshahr Uttar Pradesh
Address: Department of Geography
N.R.E.C. College Khurja, Bulandshahr Uttar Pradesh
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Papers by Atul Kumar
For hydro-geomorphological investigation, Laster Gad catchment, the tributary of Mandakini River (Rudraprayag district) in Garhwal Himalaya has been selected. The basic aim of present study is to elucidate the hydro-geomorphic characteristics of terrain through landforms mapping, geological mapping and LULC of the catchment. Beside this, the corresponding terrain attributes has been analyzed following recent geospatial techniques. It revealed that catchment has seventh order stream network with elongated shape from north to south and different homogeneous geological attributes, moderate to very steep slope and strong structural control. Bifurcation ratio between different successive orders varies very few but mean ratio (4.56) indicates that the strong structural control and less permeability of rocks. Moderate to moderate course drainage density, moderate to moderately high drainage frequency and very high texture ratio suggests that terrain has steep slopes, complex deformed lithology. Local relief of the catchment ranges from 219 m. to737 m. whereas absolute relief extent from 698 m. is in the southern part to the maximum 3770 m, in the northern part of catchment represents moderate to very high relief, less infiltration capacity and longer duration of water flow in the catchment. The morphometric indicators, existing landforms and geological formations indicate youth stage development of topography in the catchment area. Geospatial techniques and remote sensing data provide a significant help in assessing geo-hydrological studies in such terrains.
Keywords: Morphometric Analysis, Landforms, Geology and RS & GIS techniques.
For hydro-geomorphological investigation, Laster Gad catchment, the tributary of Mandakini River (Rudraprayag district) in Garhwal Himalaya has been selected. The basic aim of present study is to elucidate the hydro-geomorphic characteristics of terrain through landforms mapping, geological mapping and LULC of the catchment. Beside this, the corresponding terrain attributes has been analyzed following recent geospatial techniques. It revealed that catchment has seventh order stream network with elongated shape from north to south and different homogeneous geological attributes, moderate to very steep slope and strong structural control. Bifurcation ratio between different successive orders varies very few but mean ratio (4.56) indicates that the strong structural control and less permeability of rocks. Moderate to moderate course drainage density, moderate to moderately high drainage frequency and very high texture ratio suggests that terrain has steep slopes, complex deformed lithology. Local relief of the catchment ranges from 219 m. to737 m. whereas absolute relief extent from 698 m. is in the southern part to the maximum 3770 m, in the northern part of catchment represents moderate to very high relief, less infiltration capacity and longer duration of water flow in the catchment. The morphometric indicators, existing landforms and geological formations indicate youth stage development of topography in the catchment area. Geospatial techniques and remote sensing data provide a significant help in assessing geo-hydrological studies in such terrains.
Keywords: Morphometric Analysis, Landforms, Geology and RS & GIS techniques.