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Case Study 6




                     The Galapagos Islands




                     Volcanoes and Wildlife









                     Malcolm Cooper                             Carnegie, Cocos and Malpelso, which are on two
                                                                tectonic plates (Harpp et al, 2004). The hotspot is
                     Introduction                               located near the Equator on the Nazca Plate near
                                                                its boundary with the Cocos Plate. The tectonic
                     The Galapagos Islands are located in the Pacific   setting  of  this  hotspot  is  complicated  by  the
                     Ocean  972km  off  the  coast  of  Ecuador.  The   Galapagos Triple Junction of the Nazca and Cocos
                     isolation of the islands has permitted life forms to   plates with the Pacific Plate (Hey et al, 1972). The
                     evolve into species found only here, amongst the   movement  of  these  plates  over  the  hotspot  is
                     volcanic  landscapes. Today  the  Galapagos  Islands   therefore determined not solely by the spreading
                     are a national park and wildlife sanctuary world   along  the  ridge  but  also  by  the  relative  motion
                     heritage site. The Galapagos Archipelago consists   between  the  Pacific  Plate  and  the  Cocos  and
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                     of  7880km   of  land  spread  over  45,000km   of   Nazca plates (Harpp et al, 2002).
                             2
                     ocean in 13 main islands, 6 smaller islands and 107   Generally, the individual islands have formed
                     rocks and islets. The largest of the islands, Isabela   from  single  shield  volcano  eruptions.  However,
                     measures 4640km  and makes up half of the total   the  largest  island  Isabela  is  made  up  of  six
                                  2
                     land  area  of  the  Galapagos.  Wolf  volcano  on   volcanoes  which  have  flowed  into  each  other,
                     Isabela is the highest point with an elevation of   filling  the  gaps  between  them. The  islands  have
                     1707m above sea level.
                                                                continuously  erupted  during  the  last  200  years,
                     Geophysical aspects and                    with  the  last  eruption  being  in  2009  on
                     history of activity                        Fernandina.

                     The major volcanic islands of the archipelago are:   Risk factors
                     Genovesa  (lava  fields);  Bartolomé  (lava);  Isabela   The  Galapagos  volcanoes  remain  fairly  isolated,
                     (five  active  volcanoes);  Fernandina  (recent   but are increasingly the target of migration from
                     volcanism); Santiago (basalt lava shoreline); Santa   the  mainland.  While  active  (Wolf  volcano  has
                     Cruz (lava tubes and the Charles Darwin Research   erupted ten times since 1797) they are less of a
                     Centre); San Christobal (cinder cone, island capital   threat  to  visitors,  who  can  stay  away  while  still
                     Puerto  Baquerizo  Moreno);  Floreana  (small   experiencing  the  unique  flora  and  fauna  of  the
                     volcanic  cones).  Initially  formed  between  three   islands. Absolute risk factors for tourism are the six
                     million and five million years ago, the Galapagos   active  volcanoes  themselves,  the  nature  of  the
                     Islands are located over a hotspot in the East Pacific   resulting  land  surface  (lava  flows,  few  points  of
                     Ocean responsible for the creation of the Islands   easy  access),  overpopulation  from  approved  and
                     as  well  as  three  major  aseismic  ridge  systems,   illegal  migrants  (the ‘permanent’  population  has







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