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Case Study 18




               Geothermal Parks in


               New Zealand











               Richard Roscoe                              Zone  (Cole,  1990). This  includes  the  Ruapehu
                                                           and Tongariro volcanoes near its southern end and
               Introduction                                the  prominent  offshore  White  Island  volcano
                                                           towards  its  north-eastern  end.  Eruptions  have
               Since the advent of affordable long-haul air travel,   been recorded at each of these in the last 50 years.
               New Zealand has developed into a popular tourist   In between lie several large calderas such as Taupo,
               destination for international travellers, with over   Maroa, Okataina, Reporoa and Rotorua, together
               1.1 million foreign visitors entering the country   harbouring  the  main  geothermal  sites.  White
               for the purpose of tourism in 2008 (NZ Ministry   Island  (Figure  CS18.1)  and  the  mainland
               of  Tourism,  2009).  Further,  over  17  million   geothermal  sites  at  Rotorua,  nearby Waimangu
               domestic  tourism  trips  were  recorded.  The   Valley and Wai-O-Tapu are the focus of this case
               popularity  of  New  Zealand  can  be  largely   study.
               attributed  to  the  diversity  of  its  landscapes,   All sites have some form of protected status.
               including  the  spectacular  volcanic  landscapes  of   White Island is a designated private scenic reserve,
               the North Island as well as the alpine landscapes   with  access  only  by  permit  since  1995. Tourists
               and dramatic coastlines of the South Island with   must  use  the  authorized  helicopter  or  boat
               their  diverse  wildlife.  A  large  proportion  of   operators  to  visit  the  island.  Rotorua’s  main
               international visitors visit the geothermal areas in   geothermal field, Whakarewarewa, is in a fenced
               and  around  Rotorua,  where  the  local  economy   enclosure together with the adjacent New Zealand
               receives  one  third  of  its  income  from  the  1.5   Maori Arts  and  Crafts  Institute. The  latter  pays
               million visitors it receives annually (one third each   tribute to the fact that Rotorua remains a major
               from forestry and agriculture makes up the rest;   Maori  settlement.  Wai-O-Tapu  and  Waimangu
               Rotorua  District  Council,  2008).  For  NZ  as  a   Valley  are  both  enclosed  areas  designated  scenic
               whole, tourism represents about 9.2 per cent of   reserves  which  affords  them  protection  from
               gross domestic product (GDP), and accounts for   development.
               9.7 per cent of total employment (NZ Ministry of
               Tourism, 2009).                             Historical aspects
               Geological background                       Small-scale touristic exploitation of New Zealand’s

               and activity                                geothermal areas started in the late 19th century.
                                                           Rotorua  rapidly  developed  as  a  spa  resort  for
               New Zealand is located at a plate boundary where   European visitors after a passenger rail service to
               subduction of the Pacific Plate under the Indian-  Auckland was established in 1894 (Cooper-Erfurt
               Australasian  Plate  is  occurring.  Present-day   and  Cooper,  2009).  The  beautiful  Tudor-style
               volcanic activity is restricted to the Taupo Volcanic   Government  Bath  House  building,  which  was







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