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Journal of the Indian Society of Remote Sensing

, Volume 35, Issue 4, pp 301–312 | Cite as

Remote sensing and GIS application in change detection of the Barak River channel, N.E. India

  • J. D. Das
  • T. Dutta
  • A. K. Saraf
Article

Abstract

Rivers flowing through the alluvium invariably have very low gradient forcing the river to flow slowly in a meandering and zigzag path. Nature and intensity of meandering is governed by the geological and tectonic conditions of the river basin. Barak River in tectonically active south Assam (Northeast India) exhibits intense meandering and shifting of the river course. Topographic data of two different years and satellite images of 4 different years covering a section of the Barak River have been investigated to verify the nature of changes undergone by the river through times. This study reveals active northward shift of the river and a prominent neck-cut off in the initial part of the study area. Northward shift of the river also occurred in the area west of Silchar. But, in the western part the river has shifted both towards north and south. Oscillatory shifting in the river channel has also been noticed. The river has shown a overall northward shift which is probably due to uplift of the southern part of the Barak River valley.

Keywords

Landsat River Channel River Bank Ground Control Point Oxbow Lake 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Das Gupta, A.B. and Biswas, A.K. (2000).Geology of Assam. Geological Society of India, Bangalore, 169p.Google Scholar
  2. Ganguly, S. (1993). Stratigraphy, sedimentation and hydrocarbon prospects of Tertiary succession of Tripura and Cacher,Indian Journal of Geology,65: 145–180.Google Scholar
  3. Hooke, J.M. (1995). River channel adjustment to meander cutoffs on the River Bollin and River Dane, northwest England.Geomorphology,14: 235–253.CrossRefGoogle Scholar
  4. Lane, E.W. (1957). A study of the shape of channels formed by natural streams flowing in erodible material. U.S. Army Corps of Engineers, Missouri River Division, Sediment Series 9.Google Scholar
  5. Lattman, L.H. (1959). Geomorphology: new tool for finding oil.Oil Gas J.,57: 231–236.Google Scholar
  6. Leopold, L.B. and Wolman, M.G. (1957). River channel patterns; braided, meandering, and straight. U.S. Geol. Surv. Prof. Paper 282-B.Google Scholar
  7. Nandy, D.R. (2001).Geodynamics of northeastern India and the adjoining region. ACB Publications, Kolkata, 209p.Google Scholar
  8. Ouchi, S. (1985). Response of alluvial rivers to slow active tectonic movement.Geological Society of America Bulletin,96: 504–515.CrossRefGoogle Scholar
  9. Raj, R., Mulchandani, N., Bhandari, S., Maurya, D.M. and Chamyal, L.S. (2004). Channel shifting of a highly sinuous meandering river in alluvial plain, Vishwamitri river, Mainland Gujarat.Current Science,86: 1647–1653.Google Scholar
  10. Schumm, S.A., Dumont, J.F. and Holbrook, J.M. (2000).Active Tectonics and Alluvial Rivers. Cambridge University Press, USA, 276p.Google Scholar
  11. Tator, B.A. (1958). The aerial photograph and applied geomorphology.Photogrametric Engg.,24: 549–561.Google Scholar

Copyright information

© Springer-Verlag 2007

Authors and Affiliations

  1. 1.Department of Earthquake EngineeringIndian Institute of Technology RoorkeeRoorkeeIndia
  2. 2.Reliance Industries Ltd.India
  3. 3.Department of Earth SciencesIndian Institute of Technology RoorkeeRoorkeeIndia

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