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Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

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Plate Tectonics. Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173 The Theory of Plate Tectonics 5:3 Pg. 174-179. Inside Our Planet. Drifting Continents 5:1. - PowerPoint PPT Presentation
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Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173 The Theory of Plate Tectonics 5:3 Pg. 174-179 Plate Tectonics
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Page 1: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

Table of Contents

Drifting Continents 5:1

Pg. 164-167

Sea-Floor Spreading 5:2

Pg. 168-173

The Theory of Plate Tectonics 5:3

Pg. 174-179

Plate Tectonics

Page 2: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

Inside Our Planet

Page 3: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

Drifting Continents 5:1

Alfred Wegener, a German scientist, hypothesized that all the continents were once joined together in a single landmass and have drifted apart.

Wegener called this single landmass, or supercontinent, Pangaea.

This theory became known as Continental Drift.

http://www.agci.org/classroom/geosphere/animations/pangea-

animation.php

Page 4: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

Continental Drift

Page 5: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

Drifting Continents 5:1

Wegener used evidence from:

* Land Features

* Fossils

* Climate

His hypothesis was rejected, however, because he could not explain HOW the continents moved to their present day location.

Page 6: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

Sea-Floor Spreading 5:2

The mid-ocean ridge forms the longest chains of mountains in the world, rising up from the ocean floor.

Ocean FloorsMid-ocean ridges rise from the sea floor like stitches on the seams of a baseball.

Page 7: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

The Sea-Floor is Spreading

Page 8: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

Sea-Floor Spreading 5:2

Sea-floor spreading adds more crust to the ocean floor. At the same time, older strips of rock move outward from either side of the ridge.

Evidence for sea-floor spreading comes from:

•Pillow like lava rocks on the ocean floor

•Magnetic stripes follow similar patterns on either side of the ridge

•Ages of rocks are older further from the mid-ocean ridge

Page 9: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

Sea-Floor Spreading 5:2

In a process taking tens of millions of years, part of the ocean floor sinks back into the mantle at deep-ocean trenches in a process called subduction.

http://www.planetseed.com/files/flash/science/features/earth/livingplanet/plate_boundaries/en/index2.html?width=570&height=475&popup=true

Page 10: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

The Theory of Plate Tectonics 5:3

The theory of plate tectonics states that Earth’s plates are in slow, constant motion driven by convection currents in the mantle.

Page 11: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

Plate Tectonics

Page 12: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

Plates meet at one of three types of plate boundaries:

• Divergent

• Convergent

• Transform

The Theory of Plate Tectonics 5:3

Page 13: Table of Contents Drifting Continents 5:1 Pg. 164-167 Sea-Floor Spreading 5:2 Pg. 168-173

Ticket Out The Door

Use the index card corresponding with your number to create one question about Plate Tectonics that can be answered by another student.


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