In the vast alluvial plains of West Bengal and Orissa several deltaic plains exist, occurring in an off-lap sequence. These deltas were formed in the background of eustatic fluctuations during the Quaternary Period. They were built partly during rising sea level and pertly during stationary sea level stages. Landform analysis through aerial photographs as well as Landsat imagery interpretation, attested by field study, helped to establish the palaeogeomorphology of these Quaternary deltas. Possible mode of sedimentation during different phases of sea level fluctuations has been worked out
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Bhattacharya, Asis. 1970. Geomorphology and Quaternary geology of the Baitarani Valley area, Orissa, India. Unpublished Ph. D. thesis, Indian Institute of Technology, Kharagpur, P. 153
Mallick, Sukumar. 1971. Geomorphology and Quaternary geology of the area around Burdwan, W. Bengal. Unpublished Ph. D thesis, Indian Institute of Technology, Kharagpur, p. 133
Mallick, S. and Bhattachary, A. 1972. Quaternary delta building with particular reference to Burdwan area. Paper presented in I.I.T. Kharagpur seminar on ‘Geomorphology of Lower Ganga Basin’.
Scruton, P.C. 1960. Delta building and deltaic sequence. In : Shepard, F.P.et al. (Editors). Recent sediments, Northwest Gulf in Mexico, Am. Assoc. Petrol. Geol., Tulsa, Okla., pp. 82–102
Van Andel, T.H. and Curray, J.R. 1960. Regional aspects of modern sedimentation in Northern Gulf of Mexico and similar basins and palaeogeographic significance. Ibid, pp. 345–364
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Bhattacharya, A., Mallick, S. Palaeogeomorphic reconstruction of quaternary delta in alluvial plains of West bengal and Orissa. Journ. Ind. Soc. Photo-int. & Remote Sensing 10, 55–62 (1982). https://doi.org/10.1007/BF02990614
- Alluvial Plain
- Quaternary Period
- Bengal Basin
- Deltaic Plain
- Subaerial Part