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It is still debated what process or processes have resulted in this odd structure, though longshore drift is the most accepted hypothesis.
A fourth element of the environment in which hapua form is the strong longshore drift component.
As the ice sheets melted, sea level gradually rose and longshore drift caused a spit to form between this and other islands along the moraine.
It is a physical barrier to stop sediment transport in the direction of longshore drift (also called longshore transport).
Spits occur when longshore drift reaches a section of headland where the turn is greater than 30 degrees.
The inlet has evolved over the years due to natural processes, especially longshore drift.
Its mouth has been diverted eastwards for more than 1 km by a spit resulting from longshore drift.
The terminal groyne prevents longshore drift from bringing material to other nearby places.
This often occurs in the opposite direction to longshore drift.
Where longshore drift occurs in opposite directions, two spits merge into a triangular protrusion along a coastline or lakeshore.
There are three artificial groynes had been placed at northern part of the sandspit, to accumulate sediment from longshore drift.
Trained entrances can provide better navigation, water quality and flood mitigation services, but can also cause beach erosion due to their interruption of longshore drift.
Sediment is transported along the coast in the direction of the prevailing current (longshore drift).
In the ocean, groynes create beaches, or prevent them being washed away by longshore drift.
The sediment provided is not adequate to nourish the coast against its typical high energy waves and strong longshore drift.
