Page 125 - Volcano and Geothermal Tourism
P. 125

102    The Americas



               marked  by  a  narrow  depression  between  the   de Tucle–Loma Lucero horst and on the west by
               mountains and the sea. To the north the land rises   El Tatio volcanics (Lahsen and Trujillo, 1976; de
               and  becomes  more  arid,  until  one  reaches  the   Silva and Francis, 1991). The geothermal field at
               forbidding  Atacama  Desert,  one  of  the  most   elevations  from  4200  to  4600m  covers
                                                                           2
               inhospitable  regions  on  Earth. To  the  south  just   approximately  30km ,  but  the  majority  of  the
                                                                                          2
               the opposite transformation takes place: the land   thermal features are found within 10km , in three
               falls away, and the region between mountains and   distinct  basins  (upper,  middle  and  lower  basin).
               ocean  fades  into  the  baffling  archipelagic  maze   From here, several small colourful streams coalesce
               that  terminates  in  Chilean  Patagonia.  As  with   to  form  the  Rio  Salado  which  drains  westward
               many  other  countries  on  the  Pacific  Ocean   through  a  narrow  valley  in  the  horst  block
               coastline Chile has large geographical faults and a   forming  the  margin  of  the  graben.  Most  of  the
               high  geothermal  activity,  which  explains  the   springs are near boiling (86°C) at a neutral pH.
               existence of numerous sources of thermal waters.   Siliceous sinter deposits are found throughout the
               One  of  the  most  famous  geothermal  fields  in   field, sometimes as large cones at geyser vents or
               Chile is El Tatio.                          as terraces at springs. Runoff from El Tatio forms
                                                           the  headwaters  of  the  Calama  Basin,  where
               El Tatio geology                            recharge is dominantly from mountain snowmelt.
               The geothermal geyser field at El Tatio (Figure 7.4)
               is  located  near  the  Chile–Bolivia  border  in  the   Tourism and risk management at El Tatio
               northern  Antofagasta  province.  The  field  is   The  Geysers  del Tatio  are  located  approximately
               geologically  associated  with  the Altiplano–Puna   80km from the oasis town of San Pedro de Atacama
               volcanic  complex  in  the  north–south  trending   in northern Chile. El Tatio geysers are in a remote,
               Tatio Graben, bounded on the east by the Serrania   high altitude site (>4300m), in a largely uninhabited





































               Figure 7.4  The Tatio Geyser field near the Chile–Bolivia border is home to approximately 80 geysers







       Ch07.indd   102                                                                             3/28/2010   1:27:58 PM
   120   121   122   123   124   125   126   127   128   129   130