The ocean floor smooth and flat has the same general character as the land areas of the world: mountains, plains, channels, canyons, exposed rocks, and sediment-covered areas.
The lack of weathering and erosion in most areas, however, allows geological processes to be seen more clearly on the seafloor than.This one is referred to as the Abyssal Plain. Between the mid-ocean range and the continental uplift is the abyssal plain.
They are the main characteristics of the oceanic basin's geologic components. The plate tectonics are also situated here.the ocean floor and on the continents. There are few places where sands and mud have piled up in thick enough accumulations to become lithified, but on reefs and lagoons.
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