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Supervolcanoes
Descripción
Mind Map of summary of Supervolcanoes
Sin etiquetas
restless earth
supervolcano
supervolcanoes
geography
physical science
geography ~ restless earth
gcse
Mapa Mental por
haydena
, actualizado hace más de 1 año
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Creado por
haydena
hace alrededor de 9 años
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Resumen del Recurso
Supervolcanoes
Case Study
Yellowstone
Located in Yellowstone National Park, North America
Volcanic Features
'Old Faithful' the geyser
Boiling/bubbling mud
Hot springs
Caldera shaped not coned shaped
You can't see the edge
1000x bigger than average volcano
Multiple vents
Much bigger & more powerful than normal volcanoes
Worldwide effects if it erupted
Indications of Eruption
Huge earthquakes
Seismometers off the scale
Rising levels of CO2
Hydrothermal explosions
Harmonic Tremors
More volcanic activity
7 Known Supervolcanoes worldwide
1. Yellowstone Caldera - North Americxa
Case Study
2. Lake Toba - Indonesia
3. Taupo Caldera - New Zealand
4. Valles Caldera - New Mexico
5. Long Valley Caldera - North America
6. Aira Caldera - Japan
7. Asia
Characteristics
If a Supervolcano was to erupt it would be 1000x times bigger than the eruption of Mount St Helens
Flat
Unlike normal volcanoes which are like mountains, Supervolcanoes are flat
Big
Supervolancoes cover a large area and are much bigger than normal volcanoes
Caldera
Supervolcanoes have a Caldera a depression which forms after they erupt. Normal volcanoes just have a crater at the top
Effects
Worldwide
Air becomes polluted
Less sunlight
Ice age
Droughts
Air travel halted
Crops fail
Starvation
Death
Disease
Illness
Death
Almost all life wiped out
Nearly everything is destroyed
Resources lost
Sulphur dioxide makes atmosphere much colder
Ice age
Ash blown around
Buildings collapse
Suffocation
Death
Buried Alive
Breathing problems
USA
Lots of Ash, magma and rock
Power cuts
Water contaminated
Air hard to breathe
Storms
Pyroclastic Flows
500mph+ and 800C+
100km radius
Food, plants & animals wiped out
Millions are killed
Thousands are injured
Suphur gas poisions air
25000x3 of magma
Inhabitable
Buildings collapse
Ash
Suffocation
Death
Formation
1. Rising magma cannot escape and a large bulge appears on the surface
2. Cracks appear in the surface of the dome or bulge and gas, ash, lava and rocks erupt from the magma chamber
3. The magma chamber collapses forming a depression called a Caldera
Supervolcanoes form over Hotspots and on destructive subduction plate margins - where the Oceanic plate goes underneath the contential plate
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