mount pinatubo

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Mount Pinatubo, Philippines, June 1991

Before the eruption:

  • Not erupted since 1380 (dormant volcano)
  • Mt Pinatubo is located on the main Philippine island of Luzon
  • Area surrounding Mt Pinatubo was excellent for rice growing (weathered ash & lava).
  • Volcano monitored by the Americans from the nearby Clark Air Base using scientific equipment such as seismometers, tiltmeters and a GPS.

Cause of the eruption:

  • The Philippines lies on a destructive plate margin
  • Philippines Plate (oceanic crust) is subducted under the Eurasian Plate (continental crust)
  • The oceanic crust is turned into magma, rises, and erupts on the surface

Eruption Details

  • From 9th June 1991 there were many eruptions and earthquakes
  • Biggest eruption was around midday on 12th June 1991:
  • Explosion sent a cloud of steam and ash upto 30km into the sky (day turned to night). Volcanic bombs also thrown into the air
  • Pyroclastic flows went down the volcano slopes
  • Up to 50cm of ash fell on nearby farmland, villages and towns
  • Over 10cm fell within a 600km radius (some even reached Australia)
  • A typhoon then passed over the ash cloud. The heavy rainfall mixed with the ash in the sky, so the rain was falling as thick mud
  • A lahar was generated, which travelled as far as Angeles City (20km away)
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Short-term effects of the eruption

Injuries and Deaths:

  • The number of injuries and deaths were vastly reduced by the excellent management of the immediate situation before the eruption. It is suggested that only 6 people died directly due to the actual eruption (by pyroclastic flow.)

Buildings damaged:

  • Weight of the ash caused buildings to collapse, including 200,000 homes, a local hospital, most of the schools and many factories.

Infrastructure damaged:

  • Roads became unusable (ash and lahars), bridges were destroyed (making relief operations even more difficult); electricity was cut off (for three weeks); water supplies contaminated
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