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190    Asia



               Taal                                        eruption,  which  probably  took  place  around
               Taal volcano is a stratovolcano in Batangas province   3580BC. Taal is located about 50km (31 miles)
               on  the  island  of  Luzon.  Sometimes  nicknamed   from the capital of Manila and is also to be seen
               ‘the  world’s  smallest  volcano’, Taal  is  part  of  a   as  ‘a  volcano  inside  a  volcano’.  The  volcanic
               chain of volcanoes along the western side of the   island of Taal covers an area of about 23km², and
               island  of  Luzon,  which  were  formed  by  the   consists  of  overlapping  cones  and  craters;  47
               subduction of the Eurasian Plate underneath the   different cones and craters have been identified
               Philippine  Mobile  Belt.  Taal  produces  lavas   here.
               originated  from  a  mantle  wedge  metasomatized   Taal has erupted 34 times in the last 400 years,
               by aqueous fluid dehydrated from the subducted   causing  loss  of  life  in  the  populated  areas
               basaltic  crust,  and  melt  plus  fluid  derived  from   surrounding  the  lake,  the  current  death  toll
               subducted  terrigenous  sediment  (Castillo  and   standing  at  around  5000–6000.  The  greatest
               Newhall,  2004)  and  –  if  erupting  –  a  very   recorded  eruptions  in  historical  times  were  in
               dangerous  and  turbulent,  water-rich  mixture  of   1754 and in 1965. Although the volcano has been
               exploded bits of lava and steam. These eruptions,   quiet since 1977, it has shown signs of unrest since
               first  observed  at Taal  volcano  in  1965  are  the   1991  with  strong  seismic  activity  and  ground
               origin of base surges resembling those created by   fracturing events, as well as the formation of small
               the  underwater  detonation  of  atomic  bombs  at   mud pots and mud geysers on parts of the island.
               Bikini Atoll in the 1950s.                  Because of its proximity to populated areas and its
                  The  volcano  itself  consists  of  an  island  in   eruptive  history,  the  International Association  of
               Lake Taal (Figure 13.1), which is situated within   Volcanology and Chemistry of the Earth’s Interior
               a  caldera  formed  by  an  earlier,  very  powerful   (IAVCEI) has designated Taal a ‘decade volcano’




































               Figure 13.1  Taal volcano
               Source: Photo courtesy of Christoph Weber (Vulkanexpeditionen International (VEI), Germany)







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