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Mount St. Helens
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Mount St. Helens 18/05/1980
Info:
Located in the Cascade mountains,
Washington State, North-western USA
Before the eruption there was
2months of increased seismic activity
Causes:
Plate boundary:
It's a composite volcano formed at
a destructive plate boundary
Oceanic Juan de Fuca plate and
continental North American plate moved together
Juan de Fuca plate subducted under
the North American as it is denser
The magma created by the melting
of the plate rose through fissures in the earth's crust
It then cooled and over time Mount
St. Helens was formed
Cryptodome:
Solidified magma plugged the main
vent of the volcano
Magma went through a secondary
vent instead, creating a bulge (cryptodome) which grew 6ft bigger
everyday
Earthquake:
10,000 small earthquakes in the 2
months before the eruption
Caused by friction of the 2 plates
and magma movement
5.1 on Richter scale shook the
cryptodome free, causing Mount St. Helens to erupt laterally
(horizontally)
Effects of the eruption:
Primary:
All vegetation up to 21km away was
destroyed
24,000 animals died
57 people (including Harry Truman-
who refused to leave his house) died
Biggest landslide ever recorded
Spirit Lake filled with sediment
200 Houses destroyed
Secondary:
High unemployment as tourism and
logging industries collapsed
Flooding as river capacity
decreased due to ash build up
Fertile soils as ash increased
nutrients
Economic cost= $1.1bn
Responses:
Immediate:
Government set up 20 mile
exclusion zone
Most residents were evacuated
2 million face masks were sent
Roads cleared of ash
Long term:
Replanting of forest areas (10
million trees)
Roads rebuilt
Improved drainage- some drain
systems were blocked by ash so had to be cleared.
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Información
- Descripción
- AQA Physical Geography Mount St. Helens volcanic eruption case study
- Creado por
- a a · may 2014
- Actualizado
- 18 jul 2016
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- 93
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