tidal delta

tidal delta

[′tīd·əl ′del·tə]
(geology)
A sand bar or shoal formed in the entrance of an inlet by the action of reversing tidal currents.
References in periodicals archive ?
Flood risk of natural and embanked landscapes on the Ganges-Brahmaputra tidal delta plain.
Carbonate-rich sabkha and supratidal to subtidal carbonate tidal-flat sediments were deposited in the northern and northwestern part and silt- and sand-rich tidal delta deposition in the southern and southwestern part of the DBB.
SPELL OF THE TIGER: THE MAN-EATERS OF SUNDARBANS introduces readers to a mangrove swamp and tidal delta that lies between India and Bangladesh: the only place on earth where tigers routinely eat people.
Former flood-tide delta forms compose the broad shelf along the estuarine margin of the barrier spit, and subsequent reworking of the tidal delta d~ posits has altered most of their channel morphologies.
There are deep channels along the margins of the tidal delta through which there is a counterclockwise tidal current circulation (Psuty et a1.
Most of the shoal surface of the tidal delta as well as the shallow shelf along the inland margin of the barrier is medium sand.
Included here are a shoal in the intrajetty area, an ebb shoal seaward of the jetties, a large flood shoal contained by the sand dike, and a relict flood tidal delta on the bayside (Seabergh et al.
The predominant drift direction in the area is to the south, as evidenced by the down-drift asymmetry of the ebb tidal delta in the direction of storm-induced longshore currents (Seabergh et al.
Simultaneously, the inlet located at the western side of the Mundaka sand bar (zone 3) became deeper and the previous tidal delta at the mouth of the new (anomalous) inlet channel disappeared (zone 4).
Two areas can be differentiated: the northern area follows a NW-SE direction and contains larger bed structures, specifically flood tidal deltas and the spill-over lobes (Figs.
In a general way, we can observe that the values of velocity are higher during the flood ebb than during the flood, in the inner system, whereas in the flood tidal deltas and spill-over lobes (Bay and Mouth complex) the dominant current is the flood.
Lower currents have caused morphological changes in the tidal deltas at its mouth, which at present are developing front lobes closer to the shoreline as well as shallower tidal-channels as a result of the greater influence of swell in the swell-tide balance.