Coastal erosion in response to wave dynamics operative in Sagar Island, Sundarban delta, India

Abstract

Coastal erosion at Sagar Island of Sunderban delta, India, has been critically studied. The area is in the subtropical humid region. There are mainly three seasons viz: winter, summer and the monsoon. Different wave dynamic parameters were measured from theodolite observations with leveling staff and measuring gauges during lunar days at two sections of the western and eastern parts of the coastal zone during post-and pre-monsoons. A comparative study was made on the erosion/depositional pattern between the two sections in relation to different hydrodynamic parameters prevailing in these two sections. Plane table mapping was carried out to demarcate the different geomorphic units. The marine coastal landforms show dune ridges with intervening flats bordered by gently sloping beach on one side and a flat beach on the other side. The western part of the beach is mainly sandy; whereas the eastern part is silty and clayey with mud bank remnants. Actual field measurements indicate that the coastal dune belt has retreated to the order by about 20 m since 1985. The eastern part of the beach has lowered by about 2 m since 1985 and the western part was raised almost to the same tune. It is observed that accretion in the western and central parts of the beach took place; whereas severe erosion in the eastern part made the beach very narrow with remnants of mud banks and tree roots. Frequent embankment failures, submergence and flooding, beach erosion and siltation at jetties and navigational channels, cyclones and storm surges made this area increasingly vulnerable.

Keywords

Bay of Bengal / coastal erosion / Sagar Island / Sundarban delta / wave dynamics

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Aknowledgements

The author is grateful to the Deputy Director General, E R, and the Deputy Director General, Op: WSA, E R, Geological Survey of India for assigning him to this project, providing constant encouragement and finally for permitting him to present the paper in the conference and publish this research. Partial funds were provided by the IGCP-475 project on ‘DELTAS: Geological Modeling and Management’ to present the paper in the third International Conference held in Ho-Chi-Minh City, Vietnam during January 10-16, 2005. Constructive suggestions from Dr Katsuto Uehara of Kyushu University Kasuga, Japan, and Dr Heqing Cheng were gratefully acknowledged.

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