Where: Mount Pinatubo, Philippines, Asia
When: June 12th-15th, 1991
Type of volcano: Strato or composite volcano
Type of eruption: Explosive - the second biggest eruption this century
Deaths: 300 people died, thousands were evacuated
Mount Pinatuba had been dormant for 500 years. The first sign
that this situation might be changing occured on July 16, 1990 when a magnitude
7.8 earthquake (roughly the size of the 1906 San Francisco earthquake) struck
about 60 miles (100 kms.) northeast of Mount Pinatubo on the island of Luzon in
the Philippines. This caused the shaking and squeezing of the Earth's crust
beneath the volcano. At Mount Pinatubo, scientists recorded a landslide,
some local earthquakes, and a short-lived increase in steam emissions
from a pre-existing geothermal area, but otherwise the volcano seemed to
be undisturbed. In March and April 1991, however, magma started rising
towards the surface from more than 20 miles (32 kms.) beneath Pinatubo. This
triggered more small earthquakes and caused powerful steam explosions that
blasted three craters on the north side of the volcano. Thousands of
small earthquakes occurred beneath Pinatubo throughout April, May, and early
June 1991, and many thousand tons of noxious sulphur dioxide gas were
also emitted by the volcano.
On June 7th 1991, the first magma reached the surface of Mount Pinatubo
but because it had lost most of the gas contained in it on the way to
the surface, the magma merely oozed out to form a lava dome.
However, on June 12th, large amounts of gas-charged magma reached the surface
and exploded in the volcano's first spectacular eruption. When even more
highly gas charged magma reached Pinatubo's surface on June 15th, the volcano exploded
in a massive eruption that ejected more than 5 cu. kms. of volcanic material.
The ash cloud from this huge eruption rose 22 miles (35 kms.) into the
air. A blanket of volcanic ash and larger pumice pebbles
blanketed the countryside. Fine ash fell as far away as the Indian Ocean, and
satellites tracked the ash cloud several times around the globe. Huge
avalanches of red hot ash, gas, and pumice fragments called pyroclastic
flows roared down the sides of Mount Pinatubo, filling the deep valleys
with fresh volcanic deposits as much as 660 ft. (200 m.) thick. The eruption
removed so much magma and rock from below the volcano that the summit collapsed
to form a large volcanic depression or caldera 1.6 miles (2.5 kms.)
across.
Scientists
had been able to forecast Pinatubo's 1991 eruption and this resulted in the
saving of many lives and much property. Commercial aircraft were warned about
the hazard of the ash cloud from the June 15 eruption, and most avoided it.
Although much equipment was successfully protected, buildings on two U.S.
military bases in the Philippines--Clark Air Base and Subic Bay Naval
Station--were heavily damaged by ash. Nearly 20 million tons of sulphur
dioxide were injected into the stratosphere and the spread of this gas
cloud around the world caused global temperatures to drop temporarily
(1991-1993) by about 0.5°C. About 20,000 Aeta highlanders, who had lived on the
slopes of the volcano, were completely displaced, and most still wait in resettlement
camps for the day when they can return home. About 200,000 other people who
evacuated from the lowlands surrounding Pinatubo before and during the eruptions
have returned home but face continuing threats from lahars (mudflows)
that have already buried numerous towns, villages and fields.
Heavy Rain Leads to Erosion and Lahars
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Leading
edge of a debris flow triggered by heavy rain crashes down the Jiangjia Gully
in China. The flow front is about 5 m tall. Such debris flows are common here
because there is plenty of easily erodible rock and sediment upstream and
intense rainstorms are common during the summer monsoon season.
These
conditions commonly prevail after eruptions that kill vegetation over
extensive areas and spread loose volcanic rocks over the landscape. During
subsequent rainy seasons, swollen rivers will erode the new deposits and
sometimes generate lahars that are dangerous to people downstream. Even if no
lahars occur, the erosion can lead to frequent floods because of the
deposition of sediment along the river channels.
Pyroclastic
Flows Fill Valleys Pyroclastic flows
erupted by Mount Pinatubo profoundly changed the landscape around the volcano
by filling river valleys with hot volcanic rocks as thick as 200 m and killing
vegetation on nearby hillslopes. The pre-eruption landscape (upper photograph)
consisted of unconsolidated prehistoric pyroclastic-flow deposits that were
deeply eroded.
Pyroclastic
flows from the June 15 eruption swept down each of the volcano's river valleys
as far as 12 to 16 km (light-colored areas in lower photograph). With rainfall
averaging between 2 to 4 m per year in this part of the Philippines, most of it
falling in the monsoon season from June to October, thousands of small but
destructive lahars originated from these pyroclastic-flow deposits.
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