 stratovolcano was constructed
 
  stratovolcano was constructed primarily during the Holocene and
 
  primarily during the Holocene and contains one of the world's highest
 
  contains one of the world's highest lakes in its 400-m-wide summit crater.
 
  lakes in its 400-m-wide summit crater. The Pleistocene Juriques volcano is
 
  The Pleistocene Juriques volcano is located immediately to the SE and is
 
  located immediately to the SE and is capped by a 1.5-km-wide summit
 
  capped by a 1.5-km-wide summit crater. Archaeological ruins were
 
  crater. Archaeological ruins were found on the 5916-m-high crater rim
 
  found on the 5916-m-high crater rim of the steep-sided Volcán Licancabur,
 
  of the steep-sided Volcán Licancabur, which maintains constant 30 degree
 
  which maintains constant 30 degree slopes. The shallow freshwater
 
  slopes. The shallow freshwater summit lake is 90 m by 70 m wide and has a measured temperature of 6 degrees C,
 
  summit lake is 90 m by 70 m wide and has a measured temperature of 6 degrees C, supporting growth of planktonic fauna at nearly 6000 m altitude. Young blocky
 
  supporting growth of planktonic fauna at nearly 6000 m altitude. Young blocky andesitic lava flows with prominent levees extend up to 6 km down the NW-to-SW
 
  andesitic lava flows with prominent levees extend up to 6 km down the NW-to-SW flanks; older flows reach up to 15 km from the summit crater and are covered by
 
  flanks; older flows reach up to 15 km from the summit crater and are covered by pyroclastic-flow deposits that extend 12 km. The most recent activity from Licancabur
 
  pyroclastic-flow deposits that extend 12 km. The most recent activity from Licancabur produced flank lava flows. (Global Volcanic Program)
 
  produced flank lava flows. (Global Volcanic Program) 
 
 
 
   
 
 
   
 
 
   
 
 
   
 
 
   
 
 
   
 
 
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