- Floating Topic
- Floating Topic
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Formation of Volcanoes
- formed when magma from within the Earth's upper mantle rises up cracks or fractures in the crust
- at the surface, it erupts as lava
- it cools into solid rock
- overtime, more eruptions occur and lava keeps piling up into a volcano!
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Type of Lava
- Basaltic (fluid)
- Andesitic
- Rhyolitic (viscous)
- Silica Content
- 45%
- 52%
- 66%
- 75%
- 0
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- 0
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BASIC
- low viscousity (fluid, running), flows longer distance
- very hot: 1200 C
- takes a longer time to cool and solidify, flows long distance
- produces extensive but gently sloping landforms
- frequent eruptions but relatively gentle
- erupts lava and steam
- found at constructive plate margins, magma rises from mantle
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ACID
- viscous (thick), flows shorter distances
- less hot: 800 C
- cools and solidifies in a shorter time, flows short distance
- produces steep-rided and more localized features
- less frequent eruptions but more violent due to gas build up
- erupts ash, rocks, gas, steam, lava
- found at destructive plate margins