The area in front of Bar is dominated by an elliptical morphological high, with an intriguing, funnel-like feature on the west, and bordered to the SW by dune and sand-bar morphologies (Fig.20). Figure 21 shows and example of CHIRP records at the edge of southern montenegrinian shelf, with gassy sediments that hamper a sedimentary sequence penetrated up to 40-50m below the seabottom.
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