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What is going to happen next?
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What type of volcano is this?
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Nature’s pyrotechnics
Volcanic Eruptions Nature’s pyrotechnics
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Types of eruptions Nonexplosive Explosive
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What determines how a volcano erupts?
The answer is viscosity! What is viscosity? A fluids ability to resist flow. What changes the viscosity of a fluid? Let’s take a look.
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What is the connection with those three factors and explosive eruptions?
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Why Explosive? Silica rich magma = high viscosity
Highly viscous magma traps gasses. Trapped gas = high pressure in magma chamber. Eventually the pressure is too much and the vent is fractured and all of the rocks are ejected as pyroclastic material.
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Rhyolitic magma Highly viscous
Found at subduction zones because the magma comes from melted crust. Can lead to a caldera.
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Andesitic Magma Medium Viscosity
Volcanoes of andesite have both pyroclastic material and thick lava flows. Over time the pyroclastic flow and lava create layers = stratovolcano.
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Basaltic Magma Low viscosity Move through the vents very easily.
Gasses escape easily. Associated with divergent boundaries. Tend to form thin layers of lava.
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Water and Magma Explosion
Common on islands with volcanoes. Steam in magma expands rapidly Erupts with great force Krakatoa 1883.
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Lava Types High Viscosity = slow flow Block lava formed
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Lava Types Low Viscosity = fast flow, Pillow lava formed
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Let’s examine our lab. Which lava had the greatest silica content?
Rhyolite Which lava had the greatest viscosity? Which lava was most resistant to releasing gas?
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