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Three ways tectonic plates interact:

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Presentation on theme: "Three ways tectonic plates interact:"— Presentation transcript:

1 Three ways tectonic plates interact:
Converge (collide) Diverge (move apart) Slide past one another (“Transform Boundary”)

2 What’s Inside the Earth?

3 2 types: Ocean and Continental Crust
OCEAN crust Denser Thinner Eventually subducted Relatively young CONTINENTAL crust Less dense Thicker Rarely/never subducted Oldest crust on Earth

4 1912- Theory of Continental Drift
Continents were formed from the drifting apart of one super continent: Pangaea Alfred Wegener

5 Theory of Continental Drift
The shape of continents seemed to “fit” together

6 Found evidence of similar fossils and geological formations on different continents

7 Geologic Evidence Big flaw with this theory: How did the continents actually move?

8 Seafloor Spreading In 1962, Hess proposed seafloor spreading as the mechanism for continents to actually drift. Hess proposed that new ocean crust was being created along the Mid Ocean Ridges. As ocean crust collided with other plates, it was subducted and thus destroyed and recycled.

9 Theory of Plate Tectonics
Outer “shell” of Earth is broken into plates Plates are carried by convection cells in mantle Moving plates collide, diverge, or slide by each other

10 https://youtu.be/kwfNGatxUJI

11 Convection cells in (upper mantle) cause sea floor spreading

12

13 Convergent Boundaries
1. Continental/Oceanic Denser ocean crust is subducted (pulled) under Deep trenches, mountains, strong earthquakes Melting oceanic plates turn into magma Examples: Andes Mts. Cascade Mts.

14 Convergent Boundaries
2. Oceanic/Oceanic Slower plate is subducted (pulled under) Outcome = volcanic islands, strong earthquakes, tsunamis, deep trenches Ex: Aleutian islands (Alaska), Japan, Southeast Asia

15 Convergent Boundaries
3. Continental/Continental Continental Crust is light, so no subduction Instead, piles of crumpled, folded crust = tall mountains Examples: Himalayan Mts., Appalachian Mts., Alps

16 Himalayan Formation

17 Divergent Boundary Normal Fault Mostly below the ocean
Sea Floor Spreading - Forms new crust Example: Mid Atlantic Ridge, Rift Valley in Africa

18 Great Rift Valley- Africa

19 Age of Seafloor: Red is newest, green oldest

20 Transform Plate Boundaries
2 plates sliding in opposite directions E.g. San Andreas Fault

21 Major Tectonic Plates


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