Page 36 - Volcano and Geothermal Tourism
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Introduction  13



                        Four  main  types  of  volcanoes  are  generally   Maria/Santiaguito, Guatemala; Santorini, Greece;
                     distinguished:  shield  volcanoes,  composite  or   Taal,  Philippines; Teide,  Canary  Islands,  Spain;
                     strato-volcanoes,  cinder  cones  and  lava  domes.   Ulawun,  Papua  New  Guinea;  Unzen,  Japan;
                     Because this book is looking at the tourism side   Vesuvius, Italy).
                     of  volcanic  and  geothermal  environments  the   •   Hydrothermal  vent  or  black  smoker  –
                     following  list  also  includes  volcanic  landforms   continuously  spouting  under  water  at  high
                     that  are  of  interest  for  tourists,  in  alphabetical   temperatures enriched with minerals, first discovered
                     order  with  a  number  of  examples  for  each  of   in 1977 (commonly found along mid-ocean ridges).
                     them:                                      •   Igneous province and flood basalt – regions
                                                                   where large volcanic eruptions have deposited
                     •   Caldera [Spanish for cauldron] – formed by   thick  layers,  usually  basalt,  covering  expansive
                       the collapse of the roof of an empty magma   surface areas (Siberian Traps, Ethiopian Highlands;
                       chamber (Aso and Aira Caldera, Japan; Ngorongoro   Deccan Traps,  India;  Brazilian  Highlands;  Newer
                       Crater,  Tanzania;  Blake  River  Mega  Caldera,   Volcanic Provinces, Australia; North Atlantic Igneous
                       Canada;  Vilama  Caldera,  Argentina/Central   Province; Columbia River Plateau).
                       Andes;  Caldera  de  las  Canadas/Teide, Tenerife/  •   Island arc volcanoes – see volcanic arc.
                       Spain; Santorini, Greece; Crater Lake, Oregon).  •   Lava cave, lava tube – remaining cave which
                     •   Cinder  cones/scoria  cones  –  commonly   forms after lava flows stop and leave behind a
                       straight-sided  cone-shaped  hills  built  from   lava tunnel (tube) which can be up to several
                       airfall  deposits  of  fragmented  pyroclastic   kilometres long (Undara Volcanic National Park,
                       material such as particles from congealed lava   Australia;  Hawai‘i Volcanoes  National  Park;  Jeju
                       (Pu’u  O’o,  Hawai‘i;  Paricutin,  Mexico;  Eldfell,   Island,  Korea;  Canada;  Iceland;  Chile;  New
                       Iceland;  Red  Rock  and  Mt  Scoria,  Australia;   Zealand).
                       Wizard Island, Crater Lake/Oregon; Cerro Negro,   •   Lava  dome  –  created  by  slow  extrusion  of
                       Nicaragua; Kometsuka/Aso, Japan).           viscous lava from a volcanic vent (El Chichón,
                     •   Composite or strato-volcanoes – symmetrical   Mexico; Unzen, Tsurumi, Yufudake, Showashinzan,
                       and  steep-sided  cones  built  up  of  alternating   Japan;  Souffrière  Hills,  Montserrat;  Novarupta,
                       layers of lava, ash and other pyroclastic material   Redoubt  and  Augustine,  Alaska;  Bezymianny,
                       (Snaefellsjökull,  Iceland;  St  Helens  and  Mt  Baker,   Kamchatka, St Helens, Washington; Santa Maria,
                       Washington; Shasta, California; Mt Hood, Oregon;   Guatemala; Tarawera, New Zealand).
                       Mt  Fuji  and  Mt  Usu,  Japan;  Cotopaxi,  Ecuador;   •   Lava  lake  –  molten  lava  held  in  a  volcanic
                       Shishaldin, Alaska; Mayon, Philippines; Vesuvius and   crater;  active  lava  lakes,  especially  permanent
                       Stromboli,  Italy;  Nevado  del  Ruiz,  Colombia;   ones, are very rare (Ambrym, Vanuatu; Erta Ale,
                       Damavand, Iran; Merapi, Indonesia).         Ethiopia;  Kilauea,  Hawai‘i;  Erebus,  Antarctica;
                     •   Crater – bowl-shaped or funnel-like openings   Nyiragingo, D.R. of the Congo; Villarica, Chile).
                       at the mouth of a volcano, created by volcanic   •   Lava plateau – formed by sheets of lava flows
                       activity, e.g. summit craters, pit craters, maars,   pouring  from  fissures  and  creating  broad
                       diatremes.                                  plateaus  or  flood  basalts;  compare  igneous
                     •   Crater rows – can be produced along fissures   provinces  (Iceland,  North  America,  Argentina,
                       (Leirhnjúkur and Laki, Iceland; Waimangu Valley,   Japan, New Zealand).
                       New Zealand).                            •   Maars, tuff rings and diatremes – volcanic
                     •   Decade  volcanoes  –  selection  of  active   craters formed as a result of violent phreato-
                       volcanoes chosen for more in-depth research   magmatic  eruptions,  often  filled  with  water
                       to  raise  the  awareness  about  volcanoes  and   (Germany, Vulkaneifel; France, Auvergne; Australia,
                       their  potential  hazards  (Avachinsky-Koryaksky,   North  Queensland, Victoria  and  South Australia;
                       Kamchatka; Colima, Mexico; Etna, Italy; Galeras,   Ethiopia;  Turkey;  New  Mexico;  North  America;
                       Colombia; Mauna Loa, Hawai‘i; Merapi, Indonesia;   Alaska;  Patagonia,  South  America;  Israel;  Iran;
                       Nyiragongo, Democratic Republic of the Congo; Mt   Japan;  Indonesia;  Chile;  Bolivia;  New  Zealand;
                       Rainier,  Washington;  Sakurajima,  Japan;  Santa   Krashenninikov, Kamchatka).







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