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Volcanoes Chapter 6

Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:

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Page 1: Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:

Volcanoes Chapter 6

Page 2: Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:

Eruptions

• Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape– Magma: (#35) molten rock underground– Lava: (#36) molten rock at Earth’s surface

• Two types– Non-explosive

• calm flows of lava such as Mt. Kiluea or sea floor spreading• most common• happen over long periods, all the time

– Explosive• clouds of hot ash, debris, and gas shoot out• rarer• sudden and destructive

Page 3: Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:

Volcano Parts

Page 4: Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:

Magma

• Explosiveness of eruption depends on:– water– silica in magma– gases

• Water and CO2 remain dissolved in magma until pressure released– Like a can of soda exploding when top opened

• Magma with high silica content very stiff and can plug vent opening– Builds pressure by preventing water and other gases

from escaping

Page 5: Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:

Eruption Materials

• Lava (non explosive) – liquid rock– Aa or blocky: high viscosity, stiff, slow moving, brittle, jagged or blocks– Pahoehoe or pillow lava: low viscosity, more fluid, faster moving,

smooth

Page 6: Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:

More Eruption Materials

• Pyroclastic material (explosive) – magma hardens in the air or shatters existing rock– volcanic bombs– volcanic blocks– lapilli– volcanic ash

• Pyroclastic flows (#37)– hot ash, dust, and

gases ejected and flow rapidly downhill

Page 7: Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:

Effects

• Deaths by blast or pyroclastic flows• Ecologically damage• Climate change

– ash in upper atmosphere– blocks sunlight– Mt. Tambora in Indonesia in 1815

• 12,000 direct deaths• 80,000 deaths from hunger and disease• Food shortages in Europe and N. America next year due to

reduced sunlight and temperature• Global temperatures dropped .5 degrees C

Page 8: Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:

Types• Shield

– (#39) Repeated lava flows build up over time from non-explosive eruptions

– Gently sloping over wide area– Mauna Kea in Hawaii

• Cinder cone– (#40) Pyroclastic material builds up from moderately explosive eruptions– Steep slopes of cinder cones– Not very stable, sometimes on sides of other volcanoes– Paricutin in Mexico

• Composite (aka stratovolcano)– Most common type– (#41) Alternating flows of lava and pyroclastic material build up– Broad bases that get steeper towards top– Mt Fuji in Japan, Mt Hood, Mt Ranier, Mt St Helens, Mt Shasta

Page 9: Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:
Page 10: Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:

Other Volcanic Landforms

• Craters

• Calderas (#38)

• Lava plateaus

Page 11: Volcanoes Chapter 6. Eruptions Volcano – (#34) opening in Earth’s surface which allows gas & magma to escape –Magma: (#35) molten rock underground –Lava:

Locations

• Divergent boundary – mid ocean ridges– most volcanic activity on Earth

• Convergent boundary – subduction zones– descending oceanic crust– melting rock less dense and rises up– 80% of all land volcanoes at convergent

• Hot spots– mantle plumes far from plate boundaries– Hawaiian islands– Yellowstone