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what happens with a magma and water interaction
rapidly conversion of water to steam
what does steam do
greatly increases eruption explosivity
how can explosive magnitude be expressed
as a combination of plume height and volume
pumice
bubble filled lava, formed by depressurisation and cooling
volcanic ash
powerful explosions spray lava into air, which freezes into tiny fragments of glass
lapilli
pea to plum sized fragments of pumice or ash
blocks and bombs
larger (up to several m), made from pre-existing rock and molten rock respectively
tephra and tuff
fragmental deposits of volcanoes which are unconsolidated or transformed to rock respectively
effects of volcanic eruption
possible catastrophe and devastation on a variety of scales - effects range from immediate localised impacts on nearby landscapes and communities to global influences
pyroclastic flows (nuee ardente)
turbulent avalanches of gas, molten rock, ash and lapilli, are glowing, hot (300-800 degrees) and very fast moving (up to 300 km/h) - can travel 10's of km from a volcano - even across water
where do pyroclastic flows come from
gravitational collapse of an explosive eruption column
Mt. Pelée pyroclastic blast
a pressure wave of searing hot gas and ash - raced at up to 140m/s (500 km/h) down from Mt Pelée and through St. Pierre. This was followed by numerous pyroclastic flows à gravity-driven avalanches of gas, ash and lapilli
blast temperature
~250 to 400 degrees C. This was enough to set buildings and ships in St. Pierre ablaze. However, most of the victims were asphyxiated, not burned to death
how many deaths
~30,000 people
lateral blasts - Mt St Helens
On May 18th 1980 the mountainside finally failed and collapsed as a huge landslide, which moved down slope at 70-150 miles per hour. The landslide depressurised the magma below. This dramatic reduction in pressure caused the volcano to explode almost instantly
what highlights the power of the eruption
The dramatic change in the shape of Mt. St Helens
Mt St Helens crater
several explosive eruptions occurred at the summit, excavating a 350m wide and 150m deep crater
facts of the lateral blast
speed: ~500 km per hour
temperature: 350 degrees C
casualties: 57
thermal energy: 24 megatons
long term exposure to ash
silicosis of the lungs
ash clouds - December 15th 1989 KLM flight
descending to Anchorage Alaska, all four engines failed and had to be replaced: US$80 million in damage to the aircraft
April 14th 2010 – Iceland's Eyjafjallajökull
Cloud of ash sent over North Atlantic ocean.
>300 airports in 21 countries closed in Europe from 15th-21st April 2010
>100,000 flights cancelled, 7 million passengers affected. Losses to Airline Industry estimated at > 1.3 Billion euro
what is Indonesia known as
land of 129 active volcanoes
Indonesia’s famous volcanoes
Merapi, Krakatoa and Tambora
1815 eruption of Tambora
160 km3 of erupted tephra (pyroclastic flows and falls)
92,000 local fatalities (eruption, tsunami, famine)
1883 Krakatau
dominated by andesites, but may also have involved some basalt and dacite. The forces accumulating beneath Krakatau were so great that they created an explosion that was heard up to 2,250 miles away - created an atmospheric shockwave that circled the globe 4 times
global atmospheric and climatic effects of Krakatau
global temperatures dropped for few years by up to about 1 degree C and spectacular fiery sunsets persisted globally for three years after the eruption
1816
year without a summer in Northern Hemisphere - severe winter and unusually cold summer -> agricultural disruption, famine, food riots, etc
caldera
big circular depressions up to 100 kms across and '00 metres deep
cause of a caldera
the collapse of volcano centre into drained magma chamber
super volcanoes
volcanoes capable of the largest explosive eruptions (i.e. VEI = 8)
super volcanic eruptions volume
>= 1000 km3, emitted over the course of several days to a few weeks
Lake Toba
caldera collapse generated the 100km x 30km lake. 15cm ash over entire South Asia and a site in central India has 6m of ash
estimates of billions of tons of sulphur dioxide.
global impacts of lake Toba
decrease in average global temperatures is contentious but estimates of 3-3.5 degrees C - decades long volcanic winter
deforestation and vegetation destruction, severe drought in equatorial regions
proposed to be linked with a ‘bottle-neck’ in human population about the same time.
Santorini Greece
Minoan Tuff Eruption (1628BC) devastated Santorini and surrounding islands, with evidence of a tsunami striking north coast of Crete
Yellowstone
Eruptions at 2.1Myr, 1.2Myr, 640,000yrs
Most recent, Lava Creek tuff (300km3 ), involved up to 2m thick of rhyolite pyroclastic falls and flows
caldera produced
75x45km across