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Volcano Tourism in the Philippines  191



                     worthy  of  close  study  to  prevent  future  natural   within  the  past  millennium,  and  the  site  of  an
                     disasters (Hargrove, 1991).                aborted  geothermal  development.  Geologically
                        Taal  can  be  visited  easily  on  a  daytrip  from   Mt  Pinatubo  is  flanked  on  the  west  (and  partly
                     Manila  or  (better)  from  San  Nicolas  and Talisay,   underlain) by the Zambales Ophiolite Complex,
                     where a boat can be hired for the crossing. Bathing   an  easterly-dipping  slab  of  Eocene  ocean  crust
                     in  the  lake  might  be  dangerous  due  to  water   uplifted  during  the  Oligocene  (Villones,  1980).
                     snakes, as reported by locals. A walk on Taal Island   The oldest references to volcanic rocks from Mt
                     gives a good impression what it really means to   Pinatubo  are  accounts  of  the  19th  century,
                     stay  on  a  volcano:  ground  and  air  forming  a   describing the mineralogy and texture of pumice
                     unique torrid zone, caused by solar radiation and   in tuffs in the vicinity of Porac, Magalang and the
                     the  geothermal  energy  below  the  soles   O’Donnell River. Mt Pinatubo seems to show a
                     (Figure 13.2). To contact the volcano observatory   general trend from tholeiitic rocks on the west to
                     based  in  Talisay  before  trying  to  climb  this   slightly alkaline rocks on the east, with calcalkalaline
                     outstanding volcano is not a mistake. The Volcanic   rocks dominating the main volcanic belt (Newhall
                     Explosivity Index (VEI) of Taal has changed from   et al, 1996, pp165–166).
                     6  (3580BC  ±  200  years)  to  4  (28  September   The  first  geologic  commentary  about  Mt
                     1965). The younger eruptions of Taal had a VEI of   Pinatubo  itself  was  by  Smith  (1909)  who,  after
                     1–2 (Smithsonian Global Volcanism Program).  describing the Aglao Valley (Marella River valley)
                                                                as  once  filled  to  a  depth  of  120  to  150m  with
                     Pinatubo                                   loose  sand  and  boulders,  then  described  Mt
                     Before  2  April  1991  volcanologists  knew  Mt   Pinatubo as ‘devoid of volcanic ash (and) any of
                     Pinatubo as an inconspicuous stratovolcano, active   the usual indications of volcanic activity’. Smith




































                     Figure 13.2  A hike on the rim of the main crater of Taal, Philippines
                     Source: Photo courtesy of Christoph Weber (Vulkanexpeditionen International (VEI), Germany)







       Ch13.indd   191                                                                             4/7/2010   12:03:41 PM
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