Abstract
Chambal Badlands of central India are one of the most extensive badlands in the world, and are one of the four severely dissected landscapes within the Middle Alluvial Ganga Plains (MGAP). This extensive dissected landscape with labyrinth of winding gullies has offered refuge to outlaws for centuries. Badlands or ravines generally but not exclusively occur in semi-arid and arid areas with erodible rocks. These areas, dominated by surface erosion by overland flow and gullies, are characterized by heavily dissected terrains with steep slopes and channels separated by sharp ridges. The gullies rapidly incise and extend headward. Evidence suggests that the evolution of the badlands along the Chambal River coincided with the incision of the river as a result of the strengthening of SW monsoon in the early Holocene. Lineament controlled block uplifts might have also affected these areas causing the streams to rejuvenate, inducing widespread gullying in the region. Evidence such as ruins of former settlements, and remains of temple foundations suggests that these badlands were formed and/or rapidly extended during the recent historical period. The possibility of further expansion of the badlands in response to human interference is expected in the future.
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References
Alexander DE (1982) Difference between ‘‘Calanchi’’ and ‘‘Biancane’’ badlands in Italy. In: Bryan R, Yair A (eds) Badlands geomorphology and piping. Geobooks, Norwich, pp 71–87
Bryan RB, Jones JAA (1997) The significance of soil piping processes: inventory and prospect. Geomorphology 20:209–218
Haigh MJ (1984) Ravine erosion and reclamation in India. Geoforum 15:543–561
Harvey A (2004) Badlands. In: Goudie A (ed) Encyclopedia of geomorphology. Routledge, London, pp 45–47
Mishra MN, Vishwakarma LL (1999) Morphotectonics of the Chambal and the Yamuna valleys in the Western Marginal Gangetic Alluvial Plains. Geological Survey of India. http://www.portal.gsi.gov.in/pls/gsipub/PKG_PTL_PORTAL_LINKS.pGetCaseStudyRegion?inpRegionId=35
Pani P, Mohapatra SN (2001) Delineation and monitoring of gullied and ravine lands in a part of lower Chambal Valley, India, using remote sensing and GIS. Proc ACRS, Singapore 1:671–675
Sharma HS (1968) Genesis and pattern of ravines of the lower Chambal Valley. Geogr Rev India 30:14–24
Sinha R, Kettanah Y, Gibling MR, Tandon SK, Jain M, Bhattacharjee PS, Dasgupta AS, Ghazanfari P (2009) Craton-derived alluvium as a major sediment source in the Himalayan Foreland Basin of India. Geol Soc Am Bull 121:1596–1610
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Joshi, V.U. (2014). The Chambal Badlands. In: Kale, V. (eds) Landscapes and Landforms of India. World Geomorphological Landscapes. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-8029-2_13
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DOI: https://doi.org/10.1007/978-94-017-8029-2_13
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