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Geotourism and Public Safety in Volcanic Environments  81




































                     Figure 5.1  Hawai‘i Volcanoes National Park: German tourists beyond boundary line to see lava flows from up close



                     high-altitude  winds.  More  than  80  commercial   Deaths caused directly by lava flows are uncommon
                     aircraft  have  unexpectedly  encountered  volcanic   because  most  lava  flows  move  slowly.  However,
                     ash during flight and at airports over the past 15   tourist fatalities from direct contact with lava flows
                     years causing considerable damage to jet engines   have  been  recorded  in  Hawai‘i  (Heggie  and
                     and  infiltrating  the  air-filter  systems  of  plane   Heggie,  2004;  Heggie,  2005).  Most  of  these
                     cabins  (Casadevall,  1994;  USGS,  2009b).   fatalities  were  the  result  of  tourists  falling  into
                     Incidentally, even volcanic fumes with the absence   active  lava  and  falling  on  cooling  lava  (Heggie,
                     of tephra and ash are known to be immediately   2005).
                     corrosive to the engines of tour helicopters and   Another  threat  related  to  lava  flows  exists
                     aircraft  in  Hawai‘i,  resulting  in  a  restriction  of   when cooled lava flows are utilized for recreational
                     engine  air  intake  and  a  high  number  of  crashes   purposes such as hiking or when tourists trek over
                     and emergency landings (Heggie, 2005).     cooled lava flows in an attempt to view active lava
                                                                flows.  Severe  burns,  lacerations,  scrapes  and
                     Lava flows                                 abrasions,  and  muscle  strains  and  sprains  from
                     Lava  flows  consist  of  molten  rock  expelled  by   hiking the difficult terrain have been documented
                     volcanoes (Figure 5.1). Lava flows are extremely   (Heggie  and  Heggie,  2004;  Hawaiian  Volcano
                                o
                     hot  (700–1200 C  when  first  expelled)  and  can   Observatory, 2003).
                     flow long distances before cooling. Lava flows also
                     destroy  everything  in  their  path  (Kervyn  et  al,   Volcanic landslides and mudflows
                     2008; Chirico et al, 2009). For example, lava flows   Volcanic  landslides,  mudflows  and  pyroclastic
                     are  known  to  have  destroyed  or  caused  serious   flows  are  among  some  of  the  most  potentially
                     damage  to  international  airports  and  tourist   hazardous volcanic processes threatening tourists.
                     facilities  in Africa  and  Italy  (Behnke  and  Neri,   A volcanic landslide, also called a debris avalanche,
                     2003; Clocchiatti et al, 2004; Kervyn et al, 2008).   refers to the rapid down-slope movement of rock,







       Ch05.indd   81                                                                              3/28/2010   1:27:28 PM
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