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Geothermal Parks in New Zealand   325






































                     Figure CS18.1  Aerial View of White Island, New Zealand


                     erected in 1908, is a relic of the spa era and today   lies  at  the  northern  perimeter  of  the  Reporoa
                     houses the Rotorua Museum. Even before these   caldera, where the largest remaining sinter terraces
                     times, tourists visited the area in particular to see   were located. However, these bear no comparison
                     the stunning Pink and White sinter terraces on the   with  the  Rotomahana  terraces,  which  were
                     shores  of  Lake  Rotomahana  in  the  Okataina   comparable to terraces found today at Pamukkale
                     Volcanic  Complex,  about  25km  from  Rotorua.   in Turkey  or  at  Mammoth  Springs, Yellowstone
                     Guests  were  accommodated  at  the  small   National Park, USA.
                     Rotomahana  Hotel  in  the  Maori  village  of Te   Tourism  briefly  returned  to  the  Waimangu
                     Wairoa, and were ferried by canoe to the terraces.   Valley when in 1900 the largest geyser ever recorded
                     However, the 1886 Plinian eruption of nearby Mt   became active at Echo crater (Figure CS18.2). This
                     Tarawera  completely  reshaped  the  surrounding   erupted dark sediment-rich water up to a maximum
                     landscape, leading to a ten-fold increase in the size   height  of  several  hundred  metres,  and  led  to  a
                     of Lake Rotomahana and complete destruction of   guesthouse and several viewpoints being established
                     the terraces. The eruption was one of the largest   in  the  area.  Unfortunately,  the  geyser  stopped
                     eruptions  witnessed  by  man  in  this  area.  In  less   erupting in 1904 (Keam, n.d.).
                     than five hours, one to two cubic kilometres of   Tourism at White Island existed as early as the
                     basaltic  lava  were  erupted  from  a  fissure  which   1860s,  when  locals  or  day  trippers  from  passing
                     bisected the pre-existing rhyolite dome complex   Northern Star Company cruise ships occasionally
                     over a length of 8km, and extended a further 9km   visited the island by boat. The island was also the
                     to  the  south-west  through  the  lake  and  into   site of several small-scale sulphur mining operations
                     Waimangu Valley (Sable et al, 2006). The loss of   between 1883 and 1933. Remnants of the sulphur-
                     the  terraces  resulted  in  a  shift  of  tourism  away   processing  infrastructure  can  be  seen  today  (Pee
                     from the area towards nearby Wai-O-Tapu, which   Jay White Island Tours, n.d.).







       Ch21.indd   325                                                                             3/28/2010   1:32:27 PM
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