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Volcanoes and Earthquakes

Volcanoes and Earthquakes

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Volcanoes and Earthquakes. Weak spot in crust where molten material (magma) comes to the surface. What is a volcano?. What are plate tectonics ? theory which describes the motions of the earth’s crustal plates What causes plate tectonics ? convection currents in the mantle - PowerPoint PPT Presentation

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Page 1: Volcanoes and Earthquakes

Volcanoes and Earthquakes

Page 2: Volcanoes and Earthquakes

What is a volcano?

• Weak spot in crust where molten material (magma) comes to the surface

Page 3: Volcanoes and Earthquakes

Volcanoes and Plate Boundaries• What are plate tectonics? • theory which describes the motions of the earth’s• crustal plates • What causes plate tectonics?• convection currents in the mantle• Volcanic belts around plate boundaries• Ring of Fire

• Converging plate boundaries• Plates come together

• Diverging plate boundaries• Plates seperate

Page 4: Volcanoes and Earthquakes
Page 5: Volcanoes and Earthquakes

Hot Spot Volcanoes• Magma erupts through Earth’s crust• Can happen anywhere• Yellowstone

Page 6: Volcanoes and Earthquakes

Volcanic Eruptions• Quiet Eruptions• Low-silica, low-viscosity magma• Hawaii

• Explosive Eruptions• High-silica, high viscosity• Pyroclastic flow• Mt. St. Helens

Page 7: Volcanoes and Earthquakes

Volcano Life Cycle• Active-is erupting or may erupt at any time• Dormant- Might become active in future• Extinct- dead, unlikely to erupt again

Page 8: Volcanoes and Earthquakes

Volcano Energy• Energy comes from magma under Earth• Hot Springs- groundwater heated by magma and forms

pool• Geysers- Hot water, steam erupts from ground• Geothermal energy- water heated naturally• Used to warm houses • electricity (steam)

Page 9: Volcanoes and Earthquakes
Page 10: Volcanoes and Earthquakes

What is an earthquake?• Shaking and trembling that results from the movement of

rock beneath Earth’s surface

Page 11: Volcanoes and Earthquakes

Stress in Earth’s Crust

• Tension- stretches rock, divergent• Compression- Squeezes rock until it folds or breaks, convergent

• Shearing- rocks move in opposite directions

Page 12: Volcanoes and Earthquakes

Faults

• Normal Faults- diverge, footwall above hanging wall• Reverse Faults- Compression, hanging wall above

footwall, converge• Strike-slip Faults- plates move past each other

Page 13: Volcanoes and Earthquakes
Page 14: Volcanoes and Earthquakes

Seismic Waves

• Carry energy from an earthquake away from the focus (center) through Earth’s interior, and across surface

Page 15: Volcanoes and Earthquakes

Types of Seismic Waves• P waves- first to arrive, longitudinal waves, move in

solids and liquids• S waves- second to arrive, transverse waves, only in

solids• Surface waves- ground moves like ocean waves,

transverse waves

Page 16: Volcanoes and Earthquakes
Page 17: Volcanoes and Earthquakes

Seismograph

• Detects seismic waves• Used to map and monitor faults

Page 18: Volcanoes and Earthquakes

Damage from Earthquakes• Shaking- triggers landslides, avalanches, destroys

buildings and water mains• Liquefaction- loose, soft soil turns to mud• Aftershocks- smaller earthquakes following big

earthquake• Tsunamis- large wave