section 2: volcanic activity chapter 2: volcanoes
TRANSCRIPT
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Section 2: Volcanic Activity
Chapter 2: Volcanoes
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How magma reaches Earth’s surfaceLiquid magma is less dense than the
surrounding solid material, so it flows upward into any cracks in the rock above
During a volcanic eruption, the gasses dissolved in magma rush out, carrying the magma with them
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Inside a volcano
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Characteristics of magmaThe force of volcanic eruption depends
partly on the amount of gas dissolved in magma
Other important factors that affect an eruption: How thick or thin the magma is, the temperature and its silica content.
More silica= higher viscosity (thicker)
Less silica= lower viscosity (thinner)
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Types of volcanic eruptionsThe silica content of magma helps to
determine whether the volcanic eruption is quiet or explosive High viscosity (thick) causes an Explosive eruption
Low viscosity (thin) causes a Quiet eruption
A volcano erupts quietly if its lava flows easilyTwo types of lava produced by quiet eruptions
Pahoehoe -fast moving, hot lava (Low viscosity)
Aa -slow moving, cooler lava (High viscosity)
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Pahoehoe
Aa
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Magma rises through the lithosphere because it is less dense and it is rising through the solid rock. As the magma materials rise, the rock cracks and magma goes through.
Both quiet and explosive eruptions can cause damage far from the crater’s rim.
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3 Stages of a VolcanoActive - it will erupt or is erupting
Dormant - there is a possibility that it will erupt (may not be for a long time)
Extinct - it will not erupt
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Other types of volcanic activityHot spring: forms when groundwater
heated by nearby magma, rises to the surface and collects in a natural poolPressure can build and cause a geyser- a fountain of water and steam that erupts from the ground
Geothermal Energy: a clean, reliable energy source caused when water is heated by magma
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Geyser
Hot Spring