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Introduction  17




                     Table 1.4  Volcanic hazards
                     Type of volcanic hazard  Potential dangers and effects
                     Acid rain        Rain turns acidic when falling through clouds of volcanic gas or acid particle emissions. Eye and skin
                                      irritant, affects vegetation and water quality (Hansell et al, 2006).
                     Ash              Of all eruptive hazards ashfall can affect the most people because of the wide areas that can be covered
                                      (Blong, 1996). Ash is a collective term for fine pyroclasts of a size <2mm diameter, that can affect the
                                      respiratory and cardiovascular systems and is irritating to eyes and skin (Hansell et al, 2006). Ash can
                                      also destroy vegetation, crops, block roads, block drains, watercourses and cause damage to equipment.
                                      In large eruptions, the danger to aircraft is considerable and particles can impact on climate and weather
                                      (Chester et al, 2001).
                     Ballistics, bombs, blocks  Rocks and lava lumps ejected during major and minor eruptions causing injuries from impact and burns
                                      (Hansell et al, 2006).
                     Gas emissions    Volcanic gases present hazards to human health and vegetation. The effects of SO , HCl, CO  and H S
                                                                                        2
                                                                                                   2
                                                                                              2
                                      are at their most severe close to a volcano or a hydrothermal vent. Hydrogen sulphide (H S) also occurs
                                                                                            2
                                      near some hot springs and has caused fatalities in several countries.
                     Jökulhlaup       Icelandic name for glacier burst, causing severe flooding by melt water, when a volcano erupts
                                      underneath a glacier or an ice cap.
                     Lahar, landslide, mudslide Gravity-controlled mudflows carrying volcanic debris and ash mixed with water downhill. Dangerous
                                      because of their great speed, embedded large boulders and ability to wash away foundations of bridges
                                      and buildings. They can be triggered a long time after a volcanic eruption through heavy rainfall.
                     Lava flows       Lava flows are molten rock and generally move slowly along paths determined by topography and do not
                                      normally threaten life, because they allow time for evacuation. Lava flows cause destruction through
                                      burial and burning of property and vegetation and can cause thermal burns.
                     Laze (Lava haze)  HCl gas clouds form when lava flows enter the ocean and come in contact with seawater. Affects the
                                      respiratory system, irritates eyes and skin.
                     Pyroclastic flows  Pyroclastic flows and surges (Schmincke, 2006), can travel at several hundred km per hour and can even
                                      jump over ridges uphill. Maximum temperatures in such flows can reach over 800°C and can cause
                                      death, injury, destruction of buildings, impact damage and burial. They are usually caused by either a
                                      dome collapse or the collapse of an eruption column or a lateral blast.
                     Tephra, air fall deposits  They are created when blocks, bombs and lapilli are ejected from a volcanic eruption column or plume
                                      and can be deposited over long distances. The particle size can range from ash (<2mm) and lapilli
                                      (>2mm) to blocks and bombs (>greater than 64mm). Hazard can be severe, depending on the proximity
                                      to the volcano. Injuries and death through impact are possible.
                     Tsunami          Also known as ‘sea wave’ or ‘harbour wave’ and is caused by the displacement of water in the ocean by
                                      an earthquake or subaqueous eruption. A tsunami is not a tidal wave but can inundate vast stretches of
                                      low lying coastal areas.

                     Source: Compiled by author from various sources including Chester et al, 2001; Francis and Oppenheimer, 2004; Hansell et al, 2006


                     or steam vents, acid rain and ground deformation   the side of caution to avoid unpleasant or even life
                     can  make  for  rather  unpleasant  experiences.  In   threatening experiences.
                     some areas unreliable and unqualified tour guides   It  is  not  just  tourists  that  can  get  caught  by
                     offer  mountain  tours  with  great  views,  assuring   unexpected  eruptions;  this  has  happened  in  the
                     the tourists that there is no danger involved and   past to experienced and trained scientists working
                     halfway up the mountain everybody has to run for   on active volcanoes because essential information
                     their lives. These things have happened on various   appears to have been either misinterpreted or even
                     occasions and it is therefore paramount to err on   ignored  (Bruce,  2001),  resulting  in  the  death  of







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