Abstract
The exposed portions of the Thakuran River bed and the intertidal mid-channel bars reveal various bedforms of tidal origin. Sand flats with small and large-scale bedforms dominate throughout the downstream portion of the tidal shoals, whereas mudflats possess fewer physical structures. The presence of megaripple marks and ripple marks as bedforms indicates that the river extends to the upper part of the lower flow regime. Both the surface and internal structures are indicative of tidal influence. Surface structures like small ripple marks, linguoid ripples, megaripples, sandwaves, rill marks, rhomboid marks etc. are recognised. Internal structures like flaser and lenticular type are highly indicative of flood and ebb cycles. Zones with distinctive bedform characteristics can be delineated based on their morphological variations and orientations. Moreover, 5–15 cm-wide intertidal belts are populated by hybrid bedforms. The structures indicating modification of bedforms due to the fluctuating velocity and depth during ebb and flood periods include: (i) skewed spurs, (ii) ripplefans, (iii) flat-crested megaripples and sandwaves, (iv) dissected channels and (v) microdeltas.
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Das, G.K. (2017). Sedimentary Structures. In: Tidal Sedimentation of the Sunderban's Thakuran Basin. Springer, Cham. https://doi.org/10.1007/978-3-319-44191-7_7
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DOI: https://doi.org/10.1007/978-3-319-44191-7_7
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