The situation that is evidence of coastal uplift due to earthquake activity is "Tidal pools that are situated above the high tide line" (Option D).
Large earthquakes can cause unexpected coastline uplift. Land can be pushed up due to vertical movement on a fault. This is the sort of movement that created many of New Zealand's mountain ranges.
Land is lifted above sea level when such vertical displacement on a fault occurs near the coast.
The locked zone ruptures after an earthquake, triggering uplift near the trench and sinking further inshore.
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