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212    Europe



               attractions,  as  the  original  geyser  after  which  all   Also  in  this  region  is  the  explosion  crater
               others around the world are named.          Kerið.  It  is  a  cinder  cone  considered  to  have
                  Historically  Geysir  is  Iceland’s  most  famous   erupted  5000–6000  years  ago. Today  much  red
               tourist attraction. It is the original hot water spout   earth is visible on the inside of the crater, caused
               from  which  all  others  are  named.  It  has  had  a   by oxidation of iron in the magma (Guðmundsson,
               history  of  intermittent  eruptions  and  in  recent   2007). The  bottom  of  the  crater  is  below  the
               times earthquakes have tended to revive its activity.   groundwater table so it is often covered in water.
               Changes  in  the  activity  of  the  Geysir  and  the   As with many geological features in Iceland, the
               surrounding  geysers  are  strongly  related  to   geo-attraction is well interpreted with full signage
               earthquake  activity.  In  records  dated  1630  the   explaining its formation (Figure 14.3).
               geysers erupted so violently that the valley around
               them trembled.                              The Reykjanes peninsula
                  The neighbouring geyser Strokkur erupts to   Nowhere  on  Earth  is  the  junction  between  the
               heights  of  up  to  30m  approximately  every  five   American  and  European  tectonic  plates  in  the
               minutes. Both Geysir and Strokkur are surrounded   Earth’s crust as clear as on the Reykjanes peninsula
               by 30 much smaller geysers and hot pools in the   in the south-west. Here the plates diverge by as
               area,  including  one  called  Litli  Geysir  (Little   much as 2cm per year but the gap is constantly
               Geysir). At the geyser site there is a tourist complex   being  filled,  as  volcanoes  have  been  erupting
               which contains a Geoscience Centre housing an   regularly  throughout  Iceland’s  history  (Visit
               audiovisual  exhibition  on  geysers  and  volcanoes   Iceland, 2009). The Reykjanes peninsula is an area
               with an earthquake simulator (Figure 14.2).  of  dramatic  lava  landscapes,  geothermal  activity








































               Figure 14.2  Geysisstofa: An audiovisual exhibition on geysers and volcanoes







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