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Assessment of Flood Vulnerability at Village Level for Kandi Block of Murshidabad District, West Bengal


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1 Dumkal College, Murshidabad-742 406, India
 

Kandi block of Murshidabad district, West Bengal is situated in the Mayurakshi-Dwarka Plain. This is one of the maximum flood-affected blocks in Murshidabad. The average frequency of occurrence of floods in the last decade is 8. This study prepares a vulnerability map of Kandi block at village level combining physical, social and economic indicators of flood hazard. PCA analysis has been applied for computation of vulnerability indices. The results reveal that there is a difference in biophysical exposure and vulnerability index.

Keywords

Composite Index, Flood Vulnerability, PCA Analysis, Village-Level Assessment.
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  • Duarah, B. P. and Phukan, S., Understanding the tectonic behavior of Shillong Plateau, India using Remote Sensing Data. J. Geol. Soc. India, 2011, 77, 105–112.
  • Angelier, J. and Baruah, S., Seismotectonics in Northeast India: a stress analysis of focal mechanism solutions of earthquakes and its kinematic implications. Geophys. J. Int., 2001, 178, 303–326.
  • Evans, P., The tectonic framework of Assam. J. Geol. Soc. India, 1964, 5, 80–96.
  • Nandy, D. R., Geodynamics of Northeastern India and the Adjoining Region, ACB Publication, Kolkata, 2001, p. 209.
  • Kayal, J. R., Seismicity of northeast India and surroundings, development over the past 100 years. J. Geophys., 1998, 19, 9–34.
  • Nandy, D. R., Tectonic evolution of north-eastern India and adjoining area with special emphasis on contemporary geodynamics. Indian J. Geol., 2000, 72(3), 175–195.
  • Bilham, R. and England, P., Plateau pop-up during the great 1897 Assam earthquake. Nature, 2001, 410, 806–809.
  • Rajendran, C. P., Rajendran, K., Duarah, B. P., Baruah, S. and Earnest, A., Interpreting the style of faulting and paleoseismicity associated with the 1897 Shillong, northeast India, earthquake: implications for regional tectonism. Tectonics, 2004, 23(4), 1–12.
  • Banerjee, P., Burgmann, R., Nagarajan, B. and Apel, E., Intraplate deformation of the Indian subcontinent. Geophys. Res. Lett., 2008, 35, L18301, 1–5.
  • Chatterjee, N., Mazumdar, A. C., Bhattacharya, A. and Saikia, R. R., Mesoproterozoic granulites of the Shillong–Meghalaya Plateau: evidence of westward continuation of the Prydz Bay PanAfrican suture into Northeastern India. Precambrian Res., 2007, 152, 1–26.
  • Soil and Water Conservation Department, Government of Meghalaya. http://megsoil.gov.in/basic_inf.htm
  • Ghatak, A. and Basu, A. R., Vestiges of the Kerguelen Plume in the Sylhet Traps, northeastern India. Earth Planet. Sci. Lett., 2011, 308, 52–64.
  • Sharma, R., Gouda, H. C., Singh, R. K. and Nagaraju, B. V., Structural study of Meghalaya Plateau through aeromagnetic data. J. Geol. Soc. India, 2012, 79, 11–29.
  • Clark, M. K. and Bilham, R., Miocene rise of the Shillong Plateau and the beginning of the end for the Eastern Himalaya. Earth Planet. Sci. Lett., 2008, 269, 336–350.
  • Duarah, B. P. and Phukan, S., Seismic hazard assessment in the Jia Bhareli river catchment in eastern Himalaya from SRTMderived basin parameters, India. Nat. Hazards, 2011, 59, 367–381.
  • Rabus, B., Eineder, M., Roth, A. and Bamler, R., The Shuttle Radar Topography Mission – a new class of digital elevation models acquired by space borne radar. ISPRS J. Photogramm. Remote Sensing, 2003, 57, 241–262.
  • Strahler, A. N., Hypsometric (area–altitude) analysis of erosional topography. GSA Bull., 1952, 63, 1117–1142.
  • Rivix, River Tools (topographic and river network analysis) version 3.0, User’s guide, 2005.
  • Dowling, T. I., Richardson, D. P., O’Sullivan, A., Summerell, G. K. and Walker, I., Application of hypsometric integral and other terrain based matrices as indicators of the catchment health: a preliminary analysis. CSIRO Land and Water, Technical Report 20/98, 1998.
  • Pike, R. J. and Wilson, S. E., Elevation–relief ratio, hypsometric integral and geomorphic area–altitude analysis. Geol. Soc. Am. Bull., 1971, 82, 1079–1084.
  • Gilbert, G. K., Report on the Geology of Henry Mountains. US Geographical and geological survey of the rocky mts region US Government Printing Office, Washington, DC, 1877.
  • Radoane, M., Radoane, N. and Dumitriu, D., Geomorphological evolution of longitudinal river profiles in the Carpathians. Geomorphology, 2002, 50, 293–306.
  • Roy, S. S., A new approach to the analysis of transverse river valley profiles and implications for morph tectonics: a case study in Rajasthan. Curr. Sci., 2001, 81(1), 106–112.
  • Keller, E. A. and Pinter, N., Active Tectonics: Earthquake, Uplift, and Landscape, Prentice Hall, NJ, USA, 2002, 2nd edn, pp. 121– 147.
  • Goudie, A. S., Encyclopedia of Geomorphology, Routledge Ltd, 2004, p. 1036.
  • Islam, M. S., Shinjo, R. and Kayal, J. R., Pop-up tectonics of the Shillong Plateau in northeastern India: insight from numerical simulations. Gondwana Res., 2011; doi: 10, 1016/j.gr.2010.11.007.
  • Biswas, S. and Grasemann, B., Quantitative morphotectonics of the southern Shillong Plateau (Bangladesh/India). Aust. J. Earth Sci., 2005, 97, 82–93.
  • Bull, W. B. and McFadden, L. D., Tectonic geomorphology north and south of the Garlock fault, California. In Geomorphology in Arid Regions: Proceedings, Eight Annual Geomorphology Symposium (ed. Doehring, D. O.), SUNY Bringhamton, NY, USA, 1977, pp. 115–138.

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  • Assessment of Flood Vulnerability at Village Level for Kandi Block of Murshidabad District, West Bengal

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Authors

Swati Mollah
Dumkal College, Murshidabad-742 406, India

Abstract


Kandi block of Murshidabad district, West Bengal is situated in the Mayurakshi-Dwarka Plain. This is one of the maximum flood-affected blocks in Murshidabad. The average frequency of occurrence of floods in the last decade is 8. This study prepares a vulnerability map of Kandi block at village level combining physical, social and economic indicators of flood hazard. PCA analysis has been applied for computation of vulnerability indices. The results reveal that there is a difference in biophysical exposure and vulnerability index.

Keywords


Composite Index, Flood Vulnerability, PCA Analysis, Village-Level Assessment.

References





DOI: https://doi.org/10.18520/cs%2Fv110%2Fi1%2F81-86