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Volcanoes Chapter 6.

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Presentation on theme: "Volcanoes Chapter 6."— Presentation transcript:

1 Volcanoes Chapter 6

2 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

3 Volcano Parts

4 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

5 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

6 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

7 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

8 Types Shield Cinder cone Composite (aka stratovolcano)
(#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

9

10 Other Volcanic Landforms
Craters Calderas (#38) Lava plateaus

11 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


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