Badland ; Cuenca hidrográfica ; Erosión de los suelos ; Geomorfogénesis ; Holoceno ; India ; Lineamento ; Neotectónica ; Pleistoceno
The study area is located in the Pravara River Basin in the Western Deccan Province. Few previous studies postulated that badlands in the Western Deccan Upland Region owe their origin to the Pleistocene-Holocene climate change events. In order
local drop in the base-level, hence promoting erosion along these points to form the ravines. It is suggested that a neotectonic interpretation of apparently randomly spaced badlands development in the Western Deccan is more probable than a paleoclimatic