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The Lithosphere of Earth Igneous Processes and Volcanic Activity 1. Why study? Thermal state...

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The Lithosphere of Earth Igneous Processes and Volcanic Activity 1. Why study? • Thermal state • Thermal history • Composition of interior • Geothermal / Hazards • Comparative planetology 2. Volcanism and plate boundaries • Divergent - Continental breakup (Flood basalts) - Mid-ocean ridge • Convergent - Domes, flows, explosive, composite volcanoes • Intraplate Volcanism - Strombolian style - Hawaiian style
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Page 1: The Lithosphere of Earth  Igneous Processes and Volcanic Activity 1. Why study? Thermal state Thermal history Composition of interior Geothermal / Hazards.

The Lithosphere of Earth Igneous Processes and Volcanic Activity

1. Why study?• Thermal state• Thermal history• Composition of interior• Geothermal / Hazards• Comparative planetology

2. Volcanism and plate boundaries• Divergent

- Continental breakup (Flood basalts)- Mid-ocean ridge

• Convergent- Domes, flows, explosive, composite volcanoes

• Intraplate Volcanism- Strombolian style- Hawaiian style

Page 2: The Lithosphere of Earth  Igneous Processes and Volcanic Activity 1. Why study? Thermal state Thermal history Composition of interior Geothermal / Hazards.

The Lithosphere of Earth - Volcanism

Strombolian

Hawaiian Plinian

Page 3: The Lithosphere of Earth  Igneous Processes and Volcanic Activity 1. Why study? Thermal state Thermal history Composition of interior Geothermal / Hazards.

Volcanic Styles

Strombolian Activity

Hawaiian Activity

Plinian Activity

Dome Growth

Spatter Cone

Bubble Rise Rate > Magma Rise Rate

Cinder Cone

Magma Rise Rate > Gas Rise Rate

Produces turbulent, buoyant cloud,

Rises to great heights

Atmosphere sucked in, heated

Exit velocity high

Low viscosity gas-clast mixture

Pressure greatly exceeds atmospheric pressure

Cloud collapses to pyroclastic flows

Brittle lid

Degasses

Fracture & Growth

Viscous gas-rich magma


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