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This animation illustrates subduction of an oceanic plate beneath continental crust and the processes that can result in volcanic eruptions. Users can stop, play, fast forward and rewind the animation at any time to stress important points.

Summary

Subject keyword(s)Astronomy, Earth and space science, Earth processes, Earth science, Earth system structure, Geology, Geoscience, Physical sciences, Plate tectonics, Science, Space Science, Space sciences, Volcanoes
Grade levelMiddle School, High School, Informal Education
Intended audienceLearner
Resource typeAudio/Visual, Instructional Material
Resource formattext, text/html
RightsSee site for guidelines governing the use, restrictions and reproduction of these materials.
Copyright McDougal Littell Inc. All rights reserved.

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DLESE: Digital Library for Earth System EducationMSP2: Math and Science Pathways

Content contained within the resource

Visualization ES0902  Observe an animation of volcanism at a subduction zone. As an oceanic plate descends to hotter depths beneath the overriding plate, it is heated and releases water. The presence of hot, water-rich liquids causes the overlying rock to begin melting. The resulting magma is less dense than the surrounding rock, so it rises up toward the surface where it collects in magma chambers. Volcanic eruptions happen when magma from these chambers reaches the surface. Over millions of years, repeated eruptions build volcanic mountains on the overriding plate.   !   Click the image to see the animation. Jennifer Loomis, TERC