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The final stage in the client acceptance and continuance decision process involves:
Sea Mounts
Undersea mountains formed by volcanic activity, rising from the ocean floor but not reaching the surface.
Island Arcs
Curved chains of volcanic islands located along convergent tectonic plate boundaries, typically with deep ocean trenches on the convex side.
Abyssal Plains
Very flat, deep-sea floors found at depths between 3,000 and 6,000 meters, making up a large portion of the ocean's basin.
Oceanic Fracture Zones
Linear oceanographic features caused by the movement of tectonic plates, characterized by significant variations in depth and topography.
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