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9.3 – Actions at Plate Boundaries – Part II
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Do Now What is a subduction zone?
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Do Now What is a subduction zone?
Occurs when one oceanic plate is forced down into the mantle beneath a second plate.
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Key Words Destructive
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Vocab Words Continental Volcanic Arc Subduction Zone Trench
Volcanic Island Arc
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Convergent Boundaries
Although new lithosphere is constantly being added at the oceanic ridges, our planet is not growing larger. Earth’s total surface area remains the same. Convergent boundaries destroy lithosphere, that is why they are called destructive plate margins. As two plates slowly converge, the leading edge of one is bent downward, allowing it to slide beneath the other. Destructive plate margins where oceanic crust is being pushed down into the mantle are called subduction zones.
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Subduction Zones Occurs when ocean oceanic plate is forced down into the mantle beneath a second plate. The surface feature produced by the descending plate is an ocean trench. Convergent boundaries are controlled by the type of crust involved and the forces acting on the plate.
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Oceanic-Continental When the leading edge of a continental plate converges with an oceanic plate, the less dense continental plate remains floating. The denser oceanic slab sinks into the asthenosphere. These cause continental volcanic arcs. The Andes are an example.
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Oceanic-Continental
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Oceanic-Oceanic When two oceanic slabs converge, one descends beneath the other. This causes volcanic activity similar to what occurs at an oceanic-continental boundary. However, the volcanoes form on the ocean floor instead of the continent. This newly formed land consisting of an arc- shaped chain of small volcanic islands is called a volcanic island arc. The Aleutian Islands.
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Oceanic-Oceanic
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Continental-Continental
When a continental and a continental plate collide, they will form a complex mountain range. Ex: Himalayas
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Continental-Continental
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Transform Fault Boundary
Plates grind past each other without destroying the lithosphere. Ex: San Andreas Fault
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Group Activity Copy and label the following Figures; page 261 Figure 11, page 262 Figures 12 & 13, page 264 Figure 15.
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