UNIT SIX: Earth’s Structure  Chapter 18 Earth’s History and Rocks  Chapter 19 Changing Earth  Chapter 20 Earthquakes and Volcanoes.

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Presentation transcript:

UNIT SIX: Earth’s Structure  Chapter 18 Earth’s History and Rocks  Chapter 19 Changing Earth  Chapter 20 Earthquakes and Volcanoes

Chapter Nineteen: Changing Earth  19.1 Inside Earth  19.2 Plate Tectonics  19.3 Plate Boundaries  19.4 Metamorphic Rocks

19.3 Learning Goals  Characterize plate boundaries.  Relate geologic processes and features to specific plate boundaries.  Locate areas where certain boundaries are likely to form.

19.3 Plate boundaries  Imagine a single plate, moving in one direction on Earth’s surface.  One edge of the plate— the divergent boundary —moves away from things.  The opposite edge —the convergent boundary bumps into anything in the way.

19.3 Plate boundaries  An edge of a lithospheric plate that slides by another plate is called a transform fault boundary.

19.3 Divergent boundaries  Divergent boundaries are found in the ocean as mid-ocean ridges.  A divergent boundary is the line between two plates where they are moving apart.  This type of boundary is found over the rising plume of a mantle convection cell.

19.3 Divergent boundaries  Divergent boundaries can also be found on continents as rift valleys.  When a rift valley forms on land, it may eventually split the landmass.

19.3 Convergent boundaries  When oceanic plates collide, one subducts under the other.  This forms a valley in the ocean floor called a trench.

19.3 Convergent boundaries  What happens if an oceanic plate and a continental plate collide?  Which plate would subduct?  The oceanic plate must subduct under the continental plate.  A continental plate is simply too buoyant to subduct under an oceanic plate.

19.3 Mountains and convergent boundaries  Mountain ranges are formed when continents collide.

19.3 Mountains and convergent boundaries  What happens if an oceanic plate with a continent on it subducts under a continental plate?  The continents cannot be sucked into the trench because their granite rocks.  The two continents collide!

19.3 Transform fault boundaries  A good clue for locating transform faults is offsetting.  When seen from above, the feature will appear to make a zig-zag.

19.3 Transform fault boundaries  The San Andreas Fault is the transform fault boundary between two lithospheric plates—the Pacific Plate and the North American Plate.