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Exploring Oceans

The shape of the sea floor, from shelf to trench

  • 2 things to know
  • Component 03

Overview

Recall questions on the continental shelf and its importance to fishing, the continental slope and submarine canyons, the abyssal plain, ocean ridges and their rift valleys on the Mid-Atlantic Ridge and East Pacific Rise, ocean trenches in the Pacific, and how seamounts and flat-topped guyots form and support marine life.

What you need to know

Answer each one before you reveal it.

Your recallNot started
Key term

Why is the abyssal plain the flattest surface on Earth?

Key term

Explain how a rift valley forms along the crest of an ocean ridge.

Questions from this subtopic

Each one with the model answer underneath.

  1. 1

    What is the continental shelf?

    Model answer

    It is the gently sloping, shallow submerged margin of a continent, flooded by the sea and underlain by continental crust.

  2. 2

    To roughly what depth does the continental shelf usually extend before the sea floor steepens?

    Model answer

    It usually extends to about 200 m, where the shelf break marks the top of the continental slope.

  3. 3

    Why are continental shelves so important to fishing despite covering only a small fraction of the ocean floor?

    Model answer

    They are shallow enough for sunlight to reach the sea bed and receive nutrients from rivers and mixing, so they are highly productive and support most of the world's commercial fisheries.

  4. 4

    How does the continental slope differ from the shelf?

    Model answer

    The slope is far steeper, typically around 3° to 6°, and it descends from the shelf break to the deep ocean floor at about 3,000 m.

  5. 5

    What are submarine canyons, and where are they found?

    Model answer

    They are steep-sided valleys cut into the continental slope, eroded largely by turbidity currents carrying sediment down into deep water.

  6. 6

    Describe the abyssal plain.

    Model answer

    It is the deep, almost level floor of the ocean basin, lying at roughly 3,000 to 6,000 m and blanketed in fine sediment and biological ooze.

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