The two major regions of the ocean floor are the continental margin and the deep ocean basin. The continental shelf is the submerged extension of the continent, characterized by shallow waters, while the continental slope marks the transition between the shelf and the deep ocean, featuring a steep descent. Below the slope lies the continental rise, a more gradual incline formed by sediment accumulation. Together, these features represent a continuum from the landmass to the deep ocean, illustrating the gradual change in depth and geological characteristics of the ocean floor.
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