“…Despite the predominance of the economic effect from the appearance of MBs in this region, it is also necessary to take into account the dynamics of MBs when designing ports, marinas, offshore platforms, etc., in the vicinity of MBs formation regions in order to avoid, for example, possible siltation around coastal structures and changes in loads on them. Over the years, different aspects of MB have been studied by several researchers, viz., hydrography (Kurup and Varadachari, 1975;Nair, 1985), physical oceanography (Mathew et al, 1995;Jiang and Mehta, 1996;Tatavarti and Narayana, 2006;Samiksha et al, 2017;Muraleedharan et al, 2018), water quality characteristics (Rao et al, 1984;Balachandran, 2004), ecology (Nair et al, 1984;Martin Thompson, 1986), sedimentological (Ramachandran and Mallik, 1985;Mallik et al, 1988;Narayana et al, 2008), mineralogical (Nair and Murty, 1968;Rao et al, 1984), geochemical (Jacob and Qasim, 1974;Ramachandran, 1989;Badesab et al, 2018), hydrochemical (Nair and Balchand, 1992), and rheological (Faas, 1995;Jiang and Mehta, 1996;Shynu et al, 2017). Mathew et al (1995) stated that MB usually forms at 12 locations along the Kerala coast (Alleppy coastal zone) (Figure 1) during the SWM.…”