Page 37 - Volcano and Geothermal Tourism
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14     Introduction



               •   Mud volcanoes – similar to magma volcanoes,   •   Volcanic  field (Auckland VF,  New  Zealand;
                  they can erupt by channelling boiling water,   Oku VF, Cameroon; Tuya VF, British Columbia/
                  steam or pressurized gas to the surface. They   Canada; Clear Lake VF, California).
                  can  be  related  to  oil  and  gas  reserves  and   •   Volcanic fissure – fissure vent, fissure volcano,
                  sometimes  erupt  in  flames  (Gallagher,  2003)   linear or elongated fracture of the ground from
                  (Iran,  Indonesia,  Japan,  New  Zealand,  Russia,   which lava, pyroclastics or gas are erupting, can
                  Italy, China, Pakistan, Romania, Canada, North   be up to several kilometres long (Krafla, Eldgjá,
                  America, Colombia, Venezuela).             Laki  –  Iceland;  Hawai‘i;  Great  Rift  Valley;
               •   Moberg or tuya – see sub-glacial volcano.  Tobalchik – Kamchatka; Ethiopia; Komagatake – Japan).
               •   Pseudo  craters  –  also  known  as  rootless   •   Volcanic  rift  –  a  region  marked  by  volcanic
                  cones formed by exploding steam when lava   action, e.g. long linear cracks in the Earth’s crust
                  flows over wetlands (Skútustaðagígar, Iceland).  which occur where magma reaches the surface
               •   Rift valley – see volcanic rift.          (Ritchie and Gates, 2001) (Canary Islands; Hawai‘i;
               •   Shield volcanoes – built mainly from multi-  Iceland; East African Rift; Tonga Arc; Antarctica).
                  directional  lava  flows  of  Hawaiian  type
                  eruptions  into  gently  sloping  landforms   The volcanic features listed above include quite a
                  comparable  to  a  broad  shield  (Mauna  Loa,   few  interesting  volcanic  destinations  for  tourists,
                  Mauna Kea, Hawai‘i; Cascades, Oregon; Erta Ale,   although  not  all  of  them  are  accessible  to  the
                  Ethiopia;  Easter  Islands;  Hierro,  Canary  Islands;   general  public  –  for  example,  submarine
                  Skjaldbreiður,  Iceland;  Newer  Volcanic  Provinces,   hydrothermal vents or black smokers. Fascinating
                  Australia; Santorini, Greece; Tolbachik , Kamchatka;   as the latter are, access to these is only possible via
                  Rangitoto, New Zealand; Fernandina, Galapagos).  submersible  observation  crafts,  which  are  in  the
               •   Sub-glacial  volcano  –  table  mountain   exclusive service of science.
                  created by a volcanic eruption underneath a   Besides volcanic landforms, geothermal features
                                           –
                  glacier (Tuya Butte, Canada; Herdubreid, Iceland;   are  visual  attractions  in  their  own  right  and  are
                  Viedma, Argentina).                      commonly found either in the neighbourhood of
               •   Sub-marine  or  subaqueous  volcanoes  –   volcanoes,  both  active  and  dormant,  or  they
                  occur  frequently  along  mid-ocean  ridges,   originate  from  artesian  springs  and  bores  (e.g.
                  sometimes producing islands (Surtsey – Iceland;   Guarani Aquifer,  South America;  Great Artesian
                  Hawaiian  Emperor  Seamount  Chain;  Tonga  –   Basin, Australia). Hot springs do not need magma
                  Home Reef).                              bodies to acquire their high temperatures. As water
               •   Super  volcanoes  –  according  to  some   passes through subterranean rocks, the geothermal
                  scientists it is only a matter of time until one   temperature  gradient  combined  with  time  and
                  of them will erupt and cause a disaster of great   pressure at depth play a role in the formation of
                  magnitude (Cas, 2005; Watts, 2007) (Mt Toba,   hot  springs  rich  in  minerals  and  metallic  trace
                  Sumatra/Indonesia; Aniachak, Alaska; Taupo, New   elements.  The effects of heated rocks below the
                  Zealand; Yellowstone, Wyoming; Tambora, Indonesia;   surface can cause a number of processes, some of
                  Vilama Caldera, Argentina/Central Andes).  which  manifest  themselves  as  geothermal
               •   Volcanic arc – chain of volcanic islands, usually   phenomena such as hot springs, fumaroles, geysers,
                  with strong seismic activity related to underlying   boiling  lakes,  heated  streams  and  bubbling  mud
                  tectonic processes (Japanese island chains; Aleutian   ponds (Erfurt-Cooper and Cooper, 2009, pp130–
                  Volcanic Arc; Marianas Arc; Kuril Island Arc; Lesser   155).  Some  examples  below  highlight  the  most
                  Antilles;  Kermadic  Islands; Tonga  Islands;  Sunda   interesting geothermal features with some examples
                  Island Arc; Solomon Islands; Philippine Islands).  of destination countries:
               •   Volcanic  belt  –  region  of  volcanic  and
                  geothermal activity (Pacific Ring of Fire; Garibaldi   •   geysers (Iceland, New Zealand, USA, South and
                  VB,  Canada;  Andean  VB;  Trans-Mexican  VB;   Central America, Japan);
                  Taupo VB;  Okhotsk-Chukotka VB;  Pontide VB,   •   boiling  lakes  and  ponds  (Japan,  USA,  New
                  Turkey; Wrangell VB, Alaska; Central Iranian VB).  Zealand, Iceland);







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