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Geography

Near coral reef islands, which process maintains channel depths?

A)Tidal scouring creates deeper sections
B)Halocline stratification prevents mixing
C)Eustatic sea level decline exposes
D)Isostatic rebound uplifts the sediments

💡 Explanation

Tidal scouring maintains channel depths because it erodes sediments due to increased flow during tides; therefore, channels deepen rather than becoming shallow. Halocline stratification has related density driven flow behavior with varying effects, rather than targeted channel maintenance

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