Page 268 - (DK Eyewitness) Travel Guide - Ireland
P. 268

266      IRELAND  REGION  B Y  REGION

       6 Giant’s Causeway

       The sheer strangeness of this place and the bizarre
       regularity of its basalt columns have made the Giant’s
       Causeway the subject of numerous legends. The most
       popular tells how the giant, Finn MacCool (see pp30–31),
       laid the causeway to provide a path across the sea to
       Scotland to engage in battle with a rival Scottish giant by
       the name of Benandonner. The Giant’s Causeway attracts
       many tourists, who are taken by the busload from the
       visitors’ centre down to the shore. Nothing, however, can   Aird’s Snout
       destroy the magic of this place, with its looming grey cliffs   This nose-shaped promontory
       and shrieking gulls; paths along the coast allow you to   juts out from the 120-m (395-ft)
       escape the crowds.                      basalt cliffs that soar above the
                                               Giant’s Causeway.

        The Formation of the Causeway
               Hot lava
        Wooded         Valley
        landscape           61 million years ago:
                            In a series of massive
                            volcanic eruptions
                            molten lava poured
                            from narrow fissures in
                            the ground, filling in
        Lower               the valleys and burn ing
        basalts             the vegetation that
                            grew there.
          Limestone
                      Non-eroded
        Tholeiitic      surface  60 million years ago:
        basalt lava         This layer of tholeiitic
                            basalt lava cooled
                            rapidly. In the process
                            it shrank and cracked
                            evenly into polygonal-
         Inter-             shaped blocks, forming
        basaltic layer      columnar jointing
                            beneath the surface.

        Steam and           58 million years ago:
        gas clouds          New volcanic eruptions
                            produced further
                            lava flows. These had
                            a slightly different
        New lava            chemical composition
         flows              from earlier flows and,
                            once cool, did not
                            form such well
                            defined columns.
        Snow           Scree                   KEY
                            15,000 years ago: At
                        Ice  the end of the Ice Age,   1 Inter-basaltic layer
                            when the land was still   2 Road
                            frozen, sea ice ground
                            its way slowly past    3 Little Causeway
                            the high basalt cliffs,   4 Plant debris is trapped between
                            eroding the foreshore   the lava flows.
        Sea water           and helping to form    5 Grand Causeway
                            the Giant’s Causeway.
                                               6 Lower basalts

       For hotels and restaurants in this region see pp302–3 and pp323–5


   266-267_EW_Ireland.indd   266                            25/04/16   11:03 am
     Eyewitness Travel   LAYERS PRINTED:
     Starsight template    “UK” LAYER
     (Source v2.2)
     Date 23rd October 2012
     Size 125mm x 217mm
   263   264   265   266   267   268   269   270   271   272   273