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Ocean floor
The ocean floor
 Many of the important features of the oceans are
  hidden in deep water.
 The continental margin is the region around
  continents that includes the:
  continental shelf,
  continental slope, and
  continental rise.
The continental shelf
 Sand drifting down the steep face of a
  continental shelf cuts into the shelf just like
  streams cut into valleys.
Features of the ocean floor
 Maps can show the
  location of the
  continental shelf.
 The true ocean floor
  is called the abyssal
  plain.
 It is flat and smooth
  because a thick layer
  of sediment covers
  its features.
The deep ocean floor
            A barrier island is a low,
             sandy island that lies
             parallel to the
             shoreline.
            A bank is a low, flat
             region on the
             continental shelf.
            A seamount is a steep-
             sided mountain that
             rises from the ocean
             floor.
The deep ocean floor
 A guyot is a seamount
  that has eroded so that
  it has a flat top and is
  underwater.
 Mid-ocean ridges mark
  places where two
  tectonic plates are
  separating and new
  ocean crust is being
  made.
 Deep-ocean trenches are the deepest parts of the
  ocean.
Investigation 22C

    Global Winds and Ocean Currents
 Key Question:
  How do temperature and salinity cause ocean
   layering?
Rip Currents
 More than 80% of
 water rescues
 performed by surf
 beach lifeguards are
 due to rip currents.

 Rip currents are sometimes called riptides, or
 undertow. Learn why these two terms are
 misleading.

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Ocean floor

  • 2. The ocean floor  Many of the important features of the oceans are hidden in deep water.  The continental margin is the region around continents that includes the:  continental shelf,  continental slope, and  continental rise.
  • 3. The continental shelf  Sand drifting down the steep face of a continental shelf cuts into the shelf just like streams cut into valleys.
  • 4. Features of the ocean floor  Maps can show the location of the continental shelf.  The true ocean floor is called the abyssal plain.  It is flat and smooth because a thick layer of sediment covers its features.
  • 5. The deep ocean floor  A barrier island is a low, sandy island that lies parallel to the shoreline.  A bank is a low, flat region on the continental shelf.  A seamount is a steep- sided mountain that rises from the ocean floor.
  • 6. The deep ocean floor  A guyot is a seamount that has eroded so that it has a flat top and is underwater.  Mid-ocean ridges mark places where two tectonic plates are separating and new ocean crust is being made.  Deep-ocean trenches are the deepest parts of the ocean.
  • 7.
  • 8. Investigation 22C Global Winds and Ocean Currents  Key Question:  How do temperature and salinity cause ocean layering?
  • 9. Rip Currents  More than 80% of water rescues performed by surf beach lifeguards are due to rip currents.  Rip currents are sometimes called riptides, or undertow. Learn why these two terms are misleading.