Morphometric Analysis of Tapi Drainage Basin Using Remote Sensing and GIS Techniques

Giri, P. M.; Diwate, Pranaya; Mawale, Yadao Kumar

doi:10.1002/9781119687160.ch4

Cited by 4 publications

(23 citation statements)

References 13 publications

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“…2). The NNW fringe of the area and the eastern and the northeastern part of the area exhibit comparatively higher elevation ranging from 500 to 1000 m (Giri et al 2020).…”

Section: A Hill Shed Map Overlay By Contour Linesmentioning

confidence: 97%

“…Satpura range, in the north, Mahadeo hills, in the east, the Ajanta range and the Satmala hills, the on the south and the west by the Arabian Sea. Around 25% of the area of the Tapti river basin is covered by forest (Jain et al 2007;Raja et al 2010;Copley et al 2014;Giri et al 2020). The Tapti river basin typically is a basaltic landscape (Jain et al 2007;Copley et al 2014) III.…”

Section: Study Areamentioning

confidence: 99%

“…Some pre-processing function techniques to normalize the data were used to correct data error and noise. The sinks were removed by filling SRTM DEM data from the dataset (Giri et al 2020).…”

Section: Study Areamentioning

confidence: 99%

“…The north-northwestern fringe of the study area and the eastern-northeastern part of the area reflects 17 0 -25 0 to 25 0 -59.80 0 variations which have probably experienced tectonic disturbances. The scarp face of the Gavilgarh fault zone and Tapi north fault zone is characterised by a 3 0 -5 0 slope (Giri et al 2020). Institute of Science, BHU Varanasi, India…”

Section: B Slope Mapmentioning

confidence: 99%

“…The SRTM DEM has been used for the generation of the "Aspect map" of the area (Fig. 4) (Thomas et al 2012;Giri et al 2020).…”

Section: Aspect Mapmentioning

confidence: 99%

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Remote Sensing and GIS Based Extensive Morphotectonic Analysis of Tapti River Basin, Peninsular India

Shekhar¹,

Mawale²,

Giri³

et al. 2021

JSR

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The present study on Morphotectonics of the Tapti basin using remote sensing (RS) data and Geographic Information System (GIS) technique is an important input in deciphering the association between drainage morphometry and tectonics of the area. The basic structural elements like the established faults and other linear features of the study area were identified on the digitally processed remote sensing data and drainage pattern/morphometry was derived from the available Shuttle Radar Topography Mission, Digital Elevation Model (SRTM DEM) (90m) data. The various morphometric characters of the Tapti river basin were studied in detail. The drainage model of this area is a coarse sub-dendritic, trellis, and rectangular. The results of the preliminary morphometric analysis have been correlated with tectonic and seismotectonic characters exhibited by the study area. Overall, the morphometric and morphotectonic analysis revealed the area has periodically experienced tectonic and low order seismic instances.

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“…2). The NNW fringe of the area and the eastern and the northeastern part of the area exhibit comparatively higher elevation ranging from 500 to 1000 m (Giri et al 2020).…”

Section: A Hill Shed Map Overlay By Contour Linesmentioning

confidence: 97%