Volcanoes - Volcanoes and Plate Tectonics Volcanoes and Plate Boundaries Volcanic belts form along the boundaries of Earth’s plates.

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Presentation transcript:

Volcanoes - Volcanoes and Plate Tectonics Volcanoes and Plate Boundaries Volcanic belts form along the boundaries of Earth’s plates.

Volcanoes Volcanoes and Plate Boundaries Volcanoes often form where two oceanic plates collide or where an oceanic plate collides with a continental plate. In both situations, an oceanic plate sinks through a trench. Rock above the plate melts to form magma, which then erupts to the surface as lava. - Volcanoes and Plate Tectonics

Volcanoes Hot Spot Volcanoes A volcano forms above a hot spot when magma erupts through the crust and reaches the surface. - Volcanoes and Plate Tectonics

Volcanoes Properties of Magma Magma’s viscosity depends on its physical and chemical properties.  Magma is made of elements and of compounds, among them silica.  Viscosity depends on silica content and temperature.  The violence of the eruption depends on gas content in the lava/magma. - Volcanoes and Plate Tectonics

Volcanoes Magma Composition Magma varies in composition and is classified according to the amount of silica it contains. The graphs show the average composition of the two types of magma. - Properties of Magma

Volcanoes Magma Composition Silica, other oxides, and other solids. Reading Graphs: Study both graphs. What materials make up both types of magma? - Properties of Magma

Volcanoes Magma Composition Rhyolite-forming magma; about 70 percent. Reading Graphs: Which type of magma has more silica? About how much silica does this type of magma contain? - Properties of Magma

Volcanoes Magma Composition About 60 percent Estimating: A third type of magma has a silica content that is halfway between that of the other two types. About how much silica does this type of magma contain? - Properties of Magma

Volcanoes Magma Composition Rhyolite-forming magma would have higher viscosity because it is higher in silica. Predicting: What type of magma would have a higher viscosity? Explain. - Properties of Magma

Volcanoes Magma Reaches Earth’s Surface When a volcano erupts, the force of the expanding gases pushes magma from the magma chamber through the pipe until it flows or explodes out of the vent. - Volcanic Eruptions

Volcanoes Landforms From Lava and Ash Volcanic eruptions create landforms made of lava, ash, and other materials. These landforms include composite volcanoes, shield volcanoes, cinder cone volcanoes, and lava plateaus. - Volcanic Landforms

Volcanoes Landforms From Lava and Ash A caldera forms when an volcano’s magma chamber empties and the roof of the chamber collapses. The result is a large, bowl- shaped caldera. - Volcanic Landforms

Volcanoes Landforms From Magma Features formed by magma include volcanic necks, dikes, and sills, as well as batholiths and dome mountains. - Volcanic Landforms

Volcanoes Batholiths A batholith is a mass of rock formed when a large body of magma cools inside the crust. Several large batholiths form the core of mountain ranges in western North America. Half Dome in Yosemite National Park, California, is part of the Sierra Nevada batholith. - Volcanic Landforms

Volcanoes Composite Volcano Eruption Activity Click the Active Art button to open a browser window and access Active Art about composite volcano eruption. - Volcanic Eruptions

Volcanoes Kinds of Volcanic Eruptions Within the last 150 years, major volcanic eruptions have greatly affected the land and people around them. - Volcanic Eruptions

Volcanoes Outlining As you read, make an outline about volcanic landforms that you can use for review. Use the red headings for the main topics and the blue headings for the subtopics. Volcanic Landforms I.Landforms From Lava and Ash A.Shield Volcanoes B.Cinder Cone Volcanoes C.Composite Volcanoes D.Lava Plateaus E.Calderas F.Soils From Lava and Ash II.Landforms From Magma A.Volcanic Necks, Dikes and Sills B.Dikes and Sills C.Batholiths D.Dome Mountains III.Geothermal Activity A.Hot Springs B.Geysers C.Geothermic Energy - Volcanic Landforms