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At some continental margins, oceanic lithosphere is subducted.
First, the presence of new ocean ridges displaces seawater upward and outward across the continental margins.
Paradoxically, continental margins also are one of the world's biggest dump sites.
The characteristics of the various continental margins are shaped by a number of factors.
They are rare on continental margins that have extremely steep continental slopes or escarpments.
In fact, most of the sedimentary rocks exposed on the continents were originally deposited on continental margins; thus, even the hydrocarbon deposits found on land were formed for the most part on ancient continental margins.
Most of the underexplored (or frontier) basins are located in difficult environments, such as polar regions or submerged continental margins.
Since continental margins are the shallowest parts of the world's oceans, they are most affected by changes in sea level.
By far and away the largest mineral resources to be exploited from continental margins are oil and natural gas.
Submarine canyons act as conduits to bring sand-sized sediments from the continental margins to the deep sea.
A large variety of seaweeds inhabit the shallower continental margins and coastal areas, particularly in the North Atlantic.
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