Abstract
Neo-tectonism affected the evolution of landscape across the earth since post-Miocene. The Khari river in Lower Damodar fan delta in West Bengal similarly portrayed the imprints of neo-tectonism in the forms of rapidly changing meander geometry , deformation in long profiles, unpaired terraces, soft sediment structures (fluid escape structure and convolute ), etc. The study of meander geometry considering 142 loops (upper—92, middle—38 and lower—12) for the years 1972 (Survey of India topo-sheet) and 2017 (Google Earth images) portrayed rapidity in channel evolution in the middle and the lower stretches of the river compared to its upper counterpart as shown by the changing sinuosity index during 1972 and 2017 (upper: 0.1, middle: −0.4 and lower: −0.42), radius–wavelength ratio (upper: 0.01, middle: −0.06 and lower: −0.04), meander shape index (upper: −0.05, middle: −0.09 and lower: −0.01), and meander form index (upper: −0.02, middle: −0.17 and lower: −0.13). We found this kind of meander behaviour to be correlated with the negative Bouguer anomaly (−45 to −30 m Gal) in the middle reach. Similarly, based on SRTM DEM (30 m), we detected a break in the long profile at the middle reach underlain by a sub-surface fault. In addition, we observed unpaired terraces in the middle reach. Besides, our extensive field survey guided us to identify long continued fluid escape structure and convolute along the banks of the river and a typical sedimentary facies which proved to be tectonically controlled.
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References
Agarwal K, Singh I, Sharma M, Sharma S, Rajagopalan G (2002) Extensional tectonic activity in the cratonward parts (peripheral bulge) of the Ganga Plain Foreland Basin, India. Int J Earth Sci 91(5):897–905
AGI (2009) Glossary of geology. American Geological institute, Washington, D.C., online version. www.agiweb.org. Accessed Nov 2009
Akter J, Sarker MH, Popescu L, Roelvink D (2016) Evolution of the Bengal Delta and its prevailing processes. J Coast Res 321:1212–1226
Ashley GH (1931) Our youthful scenery. Geol Soc Am Bull 42:537–546
Bil M (2002) The identification of neotectonics based on changes of valley floor width. Landform Anal 3:77–85
Brice JC (1964) Channel patterns and terraces of the Loup rivers in Nebraska, U.S. Geological Survey, Prof. Paper 422D. In: Morisawa M (1968) Streams: their dynamics and morphology. McGraw Hill Book Co., New York, p 138
Brice JC (1984) Planform properties of meandering river. In: Elliott CM (ed) Proceedings of the conference of river meandering’83. American Society of Civil Engineers, New Orleans, Louisiana, pp 393–399
Brookfield ME (1998) The evolution of the great river systems of southern Asia during the Cenozoic India-Asia collision: rivers draining southwards. Geomorphology 22:285–312
Burbank DW, Anderson RS (2001) Tectonic geomorphology. Blackwell Scientific, Oxford, p 270
Cotton CA (1952) Geomorphology an introduction to the study of landforms. Wiley, New York, p 100
Cremon ÉH, Rossetti DD, Sawakuchi AD, Cohen MC (2016) The role of tectonics and climate in the late quaternary evolution of a Northern Amazonian River. Geomorphology 271(15), 22–39
Cunha PP et al (2005) Tectonic control of the Tejo river fluvial incision during the late Cenozoic, in Ródão—central Portugal (Atlantic Iberian border). Geomorphology 64:271–298
Das BC (2014) Two indices to measure the intensity of meander. In: Singh RB, Hassan MI (eds) Advances in geographical and environmental sciences, pp 233–246
Dar RA, Chandra R, Romshoo SA (2013) Morphotectonic and lithostratigraphic analysis of intermontane Karewa Basin of Kashmir Himalayas, India. J Mt Sci 10(1):1–15
Dey S (2014) Fluvial processes: meandering and braiding. In: Fluvial hydrodynamics. GeoPlanet: earth and planetary sciences. Springer, Berlin, Heidelberg
Ghosh S, Islam A (2016) Quaternary alluvial stratigraphy and palaeoclimatic reconstruction in the Damodar River Basin of West Bengal. In: Das B, Ghosh S, Islam A, Ismail M (eds) Neo-Thinking on Ganges-Brahmaputra Basin Geomorphology. Springer Geography. Springer, Cham
Goodbred SL Jr (2003) Response of the Ganges dispersal system to climate change: a source-to-sink view since the last interstade. Sed Geol 162(1–2):83–104
Goodbred JS, Kuhel SA (2000a) Enormous Ganges-Brahmaputra sediment load during strengthened early Holocene monsoon. Geology 28(12):1083–1086
Goodbred SL Jr, Kuhel SA (2000b) The significance of large sediment supply, active tectonism, eustasy on the margin sequence development: late quaternary stratigraphy and evolution of the Ganges-Brahmaputra Delta. Sed Geol 133(3–4):227–248
Goswami C (2011) Tectonic control on the drainage system in a piedmont region in tectonically active eastern Himalayas. Front Earth Sci. https://doi.org/10.1007/s11707-012-0297-z
Hack JT (1973a) Drainage adjustments in the Appalachians. In: Marisawa M (ed) Fluvial geomorphology. State University of New York, Binghamton, NY, pp 51–69
Hack JT (1973b) Stream profile analysis and stream-gradient index. J Res US Geol Sur 1(4):421–429
Islam A, Guchhait SK (2017) Analysing the influence of Farakka Barrage Project on channel dynamics and meander geometry of Bhagirathi river of West Bengal, India. Arab J Geosci 10(11)
Kober F, Zeilinger G, Ivy-Ochs S, Dolati A, Smit J, Kubik PW (2013) Climatic and tectonic control on fluvial and alluvial fan sequence formation in the Central Makran Range, SE-Iran. Global Planet Change 111:133–149
Lahiri S (1996) Channel pattern as signature of neotectonic movements—A Case study from Brahmaputra Valley in Assam. J Indian Soc Remote Sens 24(4):265–272
Latrubesse EM, Franzinelli E (2002) The Holocene alluvial plain of the middle Amazon River, Brazil. Geomorphology 44(3–4):241–257
Leopold LB, Langbein WB (1966) River meanders. Sci Am 214(6):60
Leopold LB, Wolman MG (1957) River channel patterns-braided, meandering and straight. U.S. Geological Survey, Prof. Paper 282B. In: Morisawa M (1968) Streams: their dynamics and morphology. McGraw Hill, New York, p 138
Leopold LB, Wolman MG (1960) River meanders. Bull Geol Soc Am 71:774. In: Julien PY (1985) Planform geometry of meandering alluivial channels. Civil Engineering Department, Engineering Research Center, Colorado State University, p 6
Leopold LB, Wolman MG, Miller JP (1964) Fluvial processes in geomorphology. W.H. Freeman and Company, San Francisco and London, p 281
Leopold LB, Wolman MG, Miller JP (1992) Fluvial processes in geomorphology. Dover Publications Inc., New York, p 281
Mats VD, Khlystov OM, Batist MD, Ceramicola S, Lomonosova TK, Klimansky A (2000) Evolution of the academician ridge accommodation zone in the central part of the baikal rift, from high-resolution reflection seismic profiling and geological field investigations. Int J Earth Sci 89(2):229–250
Miall AD (1985) Architectural element analysis: a new method of facies analysis applied to fluvial deposits. Earth Sci Rev 22:261–308
Perucca LP et al (2013). Morphotectonic and neotectonic control on river pattern in the Sierra de la Cantera piedmont, central Precordillera, province of San Juan, Argentina. Geomorphology. https://doi.org/10.1016/j.geomorph.2013.09.014
Radoane M et al (2003) Geomorphological evolution of longitudinal river profiles in the Carpathians. Geomorphology 50:293–306
Rosenau MR (2014) Tectonics of the Southern Andean intra-arc zone (38°–42°S). An unpublished PhD dissertation. Free University of Berlin, Department of Geosciences, Berlin
Rosgen DL (1994) A classification of natural rivers. Catena 22(3):169–199
Roy S, Sahu AS (2015) Quaternary tectonic control on channel morphology over sedimentary low land: a case study in the Ajay-Damodar interfluve of Eastern India 6(6):927–946
Sarkar S, Banerjee S, Chakraborty S (1995) Synsedimentary seismic signature in Mesoproterozoic Koldaha Shale, Kheinjua formation, central India. Indian J Earth Sci 22:158–164
Sarkar S, Chakraborty S, Banerjee S, Bose PK (2002) Facies sequence and cryptic imprint of sag tectonics in late Proterozoic Sirbu Shale, central India. In: Altermann W, Corcoran P (eds) Precambrian sedimentary environments: a modern approach to ancient depositional systems. Special publication of the International Association of Sedimentologists, No. 33. Blackwell Science, pp 369–382
Sarkar A, Sengupta S, McArthur JM, Ravenscroft P, Bera MK, Bhusan R et al (2009) Evolution of Ganges-Brahmaputra western Delta plain: clues from sedimentology. Quatern Sci Rev 28:2564–2581
Schumm SA (1963) Sinuosity of alluvial rivers of the great plains. Geol Soc Ma Bull 74:1089–1100. In: Morisawa M (1968) Streams: their dynamics and morphology. McGraw Hill Book Co., p 138
Schumm SA (2005) River variability and complexity. Cambridge University Press, Cambridge, p 65
Seeber L, Gornitz V (1983) River profiles along the Himalayan arc as indicators of active tectonics. Tectonophysics 92:335–367
Sen PK (1976) A study of the hydrological characteristics of the Banka Basin. Indian J Power Valley Develop, pp 353–358 (November, Calcutta)
Sen PK (1978) Evaluation of the hydrogeomorphological analysis of the Bhagirathi-Hooghly and Damadar interfluve: UGC research project. Department of Geography, The University of Burdwan
Seth A, Sarkar S, Bose PK (1990) Synsedimentary seismic activity in an immature passive margin basin, lower member of Katrol Formation, Upper Jurassic, Kutch, India. Sed Geol 68:279–291
Shahjahan M (1970) Factors controlling the geometry of fluvial meanders. Int Assoc Sci Hydrol B 15(3):13–24
Shukla UK, Bora DS, Singh CK (2009) Geomorphic positioning and depositional dynamics of river systems in lower Siwalik Basin, Kumaun Himalaya. J Geol Soc India 73:335
Silver CRP, Murphy MA, Taylor MH, Gosse J, Baltz T (2015) Neotectonics of the western Nepal fault system: implications for Himalayan strain partitioning. Tectonics 34(12):2494–2513
Sinha-Roy S (2001) Neotectonically controlled catchment capture: an example from the Banas and Chambal drainage basins, Rajasthan. Curr Sci 80(2):25
Sougnez N, Vanacker V (2011) The topographic signature of quaternary tectonic uplift in the Ardennes Massif (Western Europe). Hydrol Earth Syst Sci 15:1095–1107
Štěpančíková P et al (2008) Neotectonic development of drainage networks in the East Sudeten Mountains and monitoring of recent fault displacements (Czech Republic). Geomorphology 102:68–80
Stolum HH (2013) In: Richeson D (ed) The geometry of meandering rivers. Internet: www.divisbyzero.com-1490x718
Timar G (2003) Controls on channel sinuosity changes: a case study of the Tisza River, the Great Hungarian Plain. Quatern Sci Rev 22:2199–2207
Zámolyi et al (2010) Neotectonic control on river sinuosity at the western margin of the Little Hungarian Plain. Geomorphology 122:231–243
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Barman, S.D., Islam, A., Das, B.C., Mandal, S., Pal, S.C. (2019). Imprints of Neo-tectonism in the Evolutionary Record Along the Course of Khari River in Damodar Fan Delta of Lower Ganga Basin. In: Das, B., Ghosh, S., Islam, A. (eds) Quaternary Geomorphology in India. Geography of the Physical Environment. Springer, Cham. https://doi.org/10.1007/978-3-319-90427-6_6
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