How it works
The ocean floor is not flat. Leaving a continent it steps down from the shelf to the slope and rise, crosses the abyssal plain, climbs the mid-ocean ridge and drops into a trench.
Read the full guide
From the coast to the deep
The continental shelf lies under less than 200 m of water. At its edge the continental slope drops steeply, and the continental rise, a ramp of sediment, leads down to the abyssal plain, 3,000 to 6,000 m deep.
Mountains and trenches
Seamounts rise at least 1,000 m from the floor; a guyot is one with a flat top. The mid-ocean ridge forms where plates spread apart. Where one plate dives under another, a trench forms beside an island arc.
- Across, the drawing keeps the features in order but squeezes the distances; up and down, the depths are to one scale.
Questions and answers
What are the features of the ocean floor?
From the coast out: continental shelf, continental slope, continental rise and abyssal plain, with seamounts and guyots on the plain, the mid-ocean ridge with its rift valley, and trenches beside island arcs.
What is the difference between a seamount and a guyot?
Both are underwater mountains at least 1,000 m high, most of them old volcanoes. A seamount usually rises to a peak; a guyot has a large, flat top.
What is the deepest part of the ocean floor?
The ocean trenches, long narrow troughs where one plate dives under another. The greatest ocean depth ever measured, the Challenger Deep, lies in one of them.