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Volcano Tourism in Ethiopia and the Danakil Rift Zone   53



                     convoys. Furthermore, there is the risk of mines   Further, even today, tourist activities are beginning
                     on all tracks leading to the north, as evidenced by   to damage the fine crystalline structures at Dallol,
                     several recent incidents with injured soldiers and   which raises questions about the sustainability of
                     wrecked  cars.  Erta Ale  lies  further  to  the  south,   the  area  if  tourism  increases  without  a  sound
                     and is reached by driving cross-country through   development strategy.
                     salt  plains,  sandy  desert  areas  and  finally  over  a
                     rough  track  to  the  parking  site.  Orientation  is   References
                     difficult  at  times,  especially  when  one  of  the   Acocella, V.  (2006) ‘Regional  and  local  tectonics  at
                     frequent  sand-storms  is  encountered.  Hence,  for   Erta Ale caldera, Afar (Ethiopia)’, Journal of Structural
                     many reasons the use of reputable local agencies is   Geology, vol 28, no 10, pp1808–1820
                     advisable.  Most  international  agencies  cooperate   Barberi, F. and Varet, J. (1970) ‘The Erta Ale volcanic
                     with these, but direct bookings are possible. One   range  (Danakil  depression,  Northern  Afar,
                     of  the  most  recommendable  tourist  agencies  in   Ethiopia)’, Bulletin of Volcanology, vol 34, no 4
                     Ethiopia  is  Origin  Ethiopia  Tours  and  Travel,   Hardie,  L.  A.  (1991)  ‘The  roles  of  rifting  and
                                                                  hydrothermal CaCl brines in the origin of potash’,
                                                                                2
                     based in Addis Ababa (www.originsethiopiatours.  Annual  Review  of  Earth  and  Planetary  Sciences,
                     com).                                        pp131–168
                     Conclusions                                Holwerda, J. G. and Hutchinson, R. W. (1968) ‘Potash-
                                                                  bearing evaporites in the Danakil area, Ethiopia’,
                     A significant boost to tourist development in the   Economic Geology, vol 63, no 2, pp124–150
                     Danakil Depression would be the development of   LeGuern, F., Carbonelle, J. and Tazieff, H. (1979) ‘Erta
                     a road system. Work is in progress on a tarmac road   Ale  lava  lake:  Heat  and  gas  transfer  to  the
                     from the south as far as Lake Afdera. It is possible   atmosphere’,  Journal  of Volcanology  and  Geothermal
                     that this road will eventually be extended as far   Research, vol 6, pp27–48
                     north  as  the  Dallol  area,  especially  in  view  of   Mohr,  P.  (1960)  The  Geology  of  Ethiopia,  Poligrafico,
                                                                  Asmara, The University of Addis Ababa Press, Addis
                     renewed interest in the development of the natural   Ababa
                     resources at the site.  This could lead to a substantial   Weber, C. (2009) ‘Report on expeditions to Erta Ale
                     increase  in  tourism  in  the  area,  yet  at  the  same   and Dallol in 2002, 2008 and 2009’, www.v-e-i.de,
                     time  may  remove  much  of  its  rugged  charm.   accessed 19 July 2009






































       Ch03.indd   53                                                                              3/28/2010   1:26:54 PM
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