Page 300 - Ultimate Visual Dictionary (DK)
P. 300

GEOLOGY, GEOGRAPHY, AND METEOROLOGY

      The ocean floor                                             Bedrock                Shoreline
                                                                       CONTINENTAL-SHELF FLOOR
                                                                  exposed by
                                                                  tidal scour
       THE OCEAN FLOOR COMPRISES TWO SECTIONS: the continental
       shelf and slope, and the deep-ocean floor. The continental shelf and
                                                                                               Parallel strips
       slope are part of the continental crust, but may extend far into the ocean.
                                                                                               of  coarse
       Sloping quite gently to a depth of about 460 feet (140 m), the continental              material left
       shelf is covered in sandy deposits shaped by waves and tidal currents. At               by strong
                                                                                               tidal currents
       the edge of the continental shelf, the seabed slopes down to the abyssal
       plain, which lies at an average depth of about 12,500 feet (3,800 m). On
       this deep- ocean floor is a layer of sediment made up of clays, fine oozes
       formed from the remains of tiny sea creatures, and occasional mineral-
                                                                                                 Sand
       rich deposits. Echo-sounding and remote sensing from satellites has
                                                                                                 deposited
       revealed that the abyssal plain is divided by a system of mountain ranges,                in wavy
       far bigger than any on land—the mid-ocean ridge. Here, magma                              pattern by
                                                                                                 weaker
       (molten rock) wells up from the Earth’s interior and solidifies,                          currents
       widening the ocean floor (see pp. 58-59). As the ocean floor spreads,
       volcanoes that have formed over hot spots in the crust move away
       from their magma source; they become extinct and are increasingly
       submerged and eroded. Volcanoes eroded below sea level remain as
       seamounts (underwater mountains). In warm waters, a volcano that
       projects above the ocean surface often acquires a fringing coral reef,
       which may develop into an atoll as the volcano becomes submerged.
       FEATURES OF THE OCEAN FLOOR
         Sediment  Submarine      Continental
                   canyon         shelf          Course of                          Irregular patches of
                                                 mud river    Continental           fine sand deposited
                                                              rise                  by weakest currents

                                                                        Continental slope  Seamount
                                                                                         (underwater
                                                                                         mountain)
                                                                         Guyot (flat-topped
                                                                         seamount)               Abyssal
                                                                                                 plain






















             Continental         Ooze (sediment        Layer of          Pillow        Volcanic    Oceanic
             crust               consisting of  remains   volcanic       lava          crystalline   crust
                                 of  tiny sea creatures)  rock                         rock

     298
   295   296   297   298   299   300   301   302   303   304   305