“…Natural coastal accretion on the other hand most commonly occurs at deltaic coasts, where large quantities of fluvial sediment get distributed along the coast through littoral drift [12]. Energetic breaking waves, coastal landslides, and rockfall, as well as tidal flat formation, may also temporally prograde coastlines [12]. Anthropogenic coastal accretion encompasses artificial (beach) nourishment, artificial coastlines, land reclamation, and mangrove planting [12,27,28].…”