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By P. Blondel

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1994) have reported that the recent clay-rich mud overlies the inner part of this slope area while relict sand is abundant in the outer slope area. In this work, using multibeam data, set of pockmarks were observed close to NNW-SSE trending fault zone. , 2008). , 2003) marked in the Fig. (13b). Acoustic backscatter strength of the area ranges from -26 to -57 dB. Such backscatter variability is related to the seafloor slope, sediment type and relief (Blondel, 2009). Backscattering strengths at different water depth for each individual pockmark centre.

4, pp. 368-374. , De, Sutirtha, Chakraborty, B. & Jauhari, P. (2008). Structural highs on the western continental slope of India: Implications for regional tectonics. Geomorphology. 96, No. 1-2, pp. 48-61. Nair, R. R. (1975). Nature & origin of small scale topographic prominences on western continental shelf of India. Indian Jour. Mar. Sciences, Vol. 4, pp. 25-29. R. & Chakraborty, B. (1997). Study of multi-beam techniques for bathymetry and sea-bottom backscatter applications. Jour. Mar. Atmos.

2010). 5. Conclusions The work embodied in this article presents the detailed methods to study the important aspects of the bathymetric techniques. The historical background involved in the development of the bathymetric system is outlined. Present day bathymetric systems such as single and multi-beam echo-sounding system developments have direct impact due to Bathymetric Techniques and Indian Ocean Applications 27 current technology level. , transducer is developed significantly due to the material development taken place in last two decades.

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