Page 24 - Oceans
P. 24

139636
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                                                                                                                                   Size: 216 x 276 (Bleed5mm)
        Size: 216 x 276 (Bleed5mm)
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     22 Titles:E.Explore_Ocean (ED594)                                          1  022  000  18/04/07  1:30         NT1-5          Titles:E.Explore_Ocean (ED594)                                         1  023  000  18/04/07  1:30          NT1-5
         Hotspots and seamounts                                                            Crust
                                                                                 Dome pushed up
         Not all oceanic crust is formed at the spreading rifts of               by mantle plume
         midocean ridges. The hot mantle of the Earth is dotted
                                                                                 Mantle
         with extra-hot regions known as mantle plumes. Many                  plume rises
                                                                            from near core
         of these lie well away from the boundaries between the
         plates of the Earth’s crust. They form stationary hotspots            Mantle
         that burn through the crust, erupting molten lava that

         builds up into volcanoes. As each volcano is carried away
         from the hotspot by the moving crust it becomes extinct,             Core
         and another volcano erupts over the hotspot. This process

         has created chains of volcanic islands and thousands of
                                                                                ≤ Mantle pluMes
         submerged volcanoes known as seamounts.                                The mantle plumes that cause hotspots probably rise from
                                                                                deep in the mantle near the Earth’s core. Each plume pushes
                                                                                up a broad dome in the oceanic crust— 600 miles (1,000 km)
                                                                                across and 1 mile (1.6 km) high in the case of Hawaii—and an
                                                                                even higher volcano erupts from the center of the dome.


                                                                           < Volcanic cHains
                                                                           The hotspot burns a hole through the Earth’s crust,
                                                                           creating a volcano (A). But the mobile crust carries the
              a                     b     a               c      b     a   volcano away from the hotspot, so it becomes extinct and
                                                                           starts sinking. A new one erupts (B), but that is also slowly
                                                                           carried off the hotspot, too. By the time a third volcano
                                                                           appears (C), the oldest may have sunk below the waves.
         1  First volcano      2  Volcano drifts off hotspot   3  Extinct volcanoes
           erupts over hotspot   and becomes extinct   slowly sink as another
           to create an island   while a new one erupts  volcano erupts







                                                                                                        hotspots










                                                       ≤ Hawaii
                                                       The islands of Hawaii, seen here from space, have been created by
                                                       the Pacific Ocean plate slipping northwest over a hotspot at about
                                                       3 in (9 cm) a year. The hotspot is currently beneath the highly active
                                                       volcano on the biggest southeastern island. Meanwhile, the extinct
                                                       volcanoes to the north are slowly sinking, and will become progressively
                                                       smaller until they dwindle to a long chain of submerged seamounts.

                                                              < fire fountains
                                                              The volcanoes of Hawaii are huge domes that rise from the ocean floor.
                                                               The largest, Mauna Loa, is higher from base to summit than Mount
                                                                Everest in the Himalayas. Kilauea, on the flanks of Mauna Loa, is the
                                                                 most active volcano on Earth, constantly erupting fire fountains of
                                                                  fluid basalt lava that flow down to the sea in rivers of molten rock.
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