Following severe coastal retreat along the Barrier-Lagoon coastline of Southwestern Nigeria, rigid concrete groynes were installed perpendicular to the shoreline. While sand accumulated on the up-drift side of the structures, beaches located further east experienced rapid sediment loss and accelerated landward erosion. What primary geomorphic process explains this unintended environmental hazard?
- Interruption of the eastward longshore drift, which traps sediment on the up-drift side and starves down-drift coastlines of natural sand replenishmentCevap
- BGravitational down-slope displacement of marine sediments triggered by localized mass wasting in mangrove mudflats
- CDisplacement of the South-West Monsoon winds, which alters the local boundary between the rainforest and Guinea savanna zones
- DReallocation of regulatory oversight from NOSDRA to NESREA, which delayed maintenance dredging operations
Cevap
Interruption of the eastward longshore drift, which traps sediment on the up-drift side and starves down-drift coastlines of natural sand replenishment
Along the Barrier-Lagoon coast of Southwestern Nigeria (such as the Lagos shoreline), prevailing waves from the Atlantic Ocean approach obliquely, driving longshore drift from west to east. Constructing groynes perpendicular to the shore traps sand on the western (up-drift) side. Because the sediment supply moving down the coast is blocked, waves hitting the eastern (down-drift) side continue to carry sand away without receiving replenishment, resulting in severe accelerated coastal erosion.
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Coastal Erosion Hazards and Shoreline Management Dynamics in Nigeria
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