1992
DOI: 10.1007/bf03001917
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Hydromorphogeological studies around Pinjaur-Morni-Kala Amb area, Ambala district (Haryana), and Sirmur district (Himachal Pradesh)

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Cited by 15 publications
(6 citation statements)
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“…The geomorphology map of the study area was prepared using LISS III satellite image through visual interpretation. Remote sensing provides an opportunity for better observation and analysis of various hydrogeomorphic features following the synoptic, multispectral repetitive coverage of the terrain (Horton 1945;Kumar and Srivastava 1991;Sharma and Jugran 1992). The various landforms delineated in the study area are classified as pediplain moderately weathered, pediplain shallow weathered, pediment-inselberg complex, flood plain, plateau weathered moderate, plateau weathered shallow, pediment, inselberg, alluvial plain, and river/waterbody/sand.…”
Section: Geomorphologymentioning
confidence: 99%
“…The geomorphology map of the study area was prepared using LISS III satellite image through visual interpretation. Remote sensing provides an opportunity for better observation and analysis of various hydrogeomorphic features following the synoptic, multispectral repetitive coverage of the terrain (Horton 1945;Kumar and Srivastava 1991;Sharma and Jugran 1992). The various landforms delineated in the study area are classified as pediplain moderately weathered, pediplain shallow weathered, pediment-inselberg complex, flood plain, plateau weathered moderate, plateau weathered shallow, pediment, inselberg, alluvial plain, and river/waterbody/sand.…”
Section: Geomorphologymentioning
confidence: 99%
“…Remote-sensing studies provide an opportunity for better observation and more systematic analysis of various hydrogeomorphic units, lineaments, features following the synoptic, multispectral repetitive coverage of the terrain (Horton 1945;Kumar and Srivastava 1991;Sharma and Jugran 1992;Chatterjee and Bhattacharya 1995;Tiwari and Rai 1996). A number of hydrogeomorphic units have been identified in this region using IRS LISS III images (Fig.…”
Section: Hydrogeomorphologymentioning
confidence: 99%
“…Geomorphology of an area is one of the most important features in evaluating the groundwater potential and prospect (Das et al 1997;Kumar et al 2008). Remote-sensing studies provide an opportunity for better observation and more systematic analysis of various hydrogeomorphic units/ landforms/lineaments, features following the synoptic, multispectral repetitive coverage of the terrain (Horton 1945;Kumar and Srivastava 1991;Sharma and Jugran 1992;Chatterjee and Bhattacharya 1995;Tiwari and Rai 1996). The geomorphic evolution of the hard rock terrain is controlled by mainly tectonic-lithologic features and denudational processes.…”
Section: Hydrogeomorphologymentioning
confidence: 99%