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Plate Tectonics By: Davon and Whitney. Vocabulary Crust Mantle Core Lithosphere Asthenosphere Mesosphere Outer core Inner core Tectonic plate Continental.

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Presentation on theme: "Plate Tectonics By: Davon and Whitney. Vocabulary Crust Mantle Core Lithosphere Asthenosphere Mesosphere Outer core Inner core Tectonic plate Continental."— Presentation transcript:

1 Plate Tectonics By: Davon and Whitney

2 Vocabulary Crust Mantle Core Lithosphere Asthenosphere Mesosphere Outer core Inner core Tectonic plate Continental drift Sea-floor spreading Convergent boundary Subuction zone Divergent boundary Transform boundary Stress Compression Tension Folding Fault Normal fault Reverse fault Strike-slip fault

3 Vocabulary Sea-floor spreading Convergent boundary Seduction zone Divergent boundary Transform boundary Stress Compression Tension Folding Fault Normal fault Reverse fault Strike-slip fault

4 Tectonic Plate Boundaries

5 Sea floor Sea-floor spreading creates new oceanic lithosphere at mid- ocean ridges.

6 Pangaea

7 Structure of the earth

8 Vocabulary Review Asthenosphere- the soft layer of the mantle on which pieces of the lithosphere move Plate tectonics- the theory that the earths lithosphere is divided into tectonic plates that move around on top of the asthensphee Folding-the bending of rock layers due to stress in the earths crust Convergent boundary-the boundary between two colliding tectonic plates

9 Vocabulary Review Sea-floor spreading- the process by which new oceanic lithosphere is created at mid-ocean ridges as older materials are pulled away from the ridge. Crust- the thin, outermost layer of the earth, or the uppermost part of the lithosphere. Seduction zone-the region where an oceanic plate sinks down into the asthenosphere at a convergent boundary, usually between continental and oceanic plate

10 Vocabulary Review Stress- the amount of force per unit area that is put on a given material. Tension- the type of stress that occurs when forces act to stretch an object. Reverse fault- a fault in which the hanging wall moves up relative to the footwall.


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