Plate Tectonics Chapter 9 2 9 3 Plate

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Plate Tectonics Chapter 9. 2 – 9. 3

Plate Tectonics Chapter 9. 2 – 9. 3

Plate Tectonics • Proposed in 1965 by Tuzo Wilson = combination of Wegener &

Plate Tectonics • Proposed in 1965 by Tuzo Wilson = combination of Wegener & Hess’s ideas. • Convection Currents move the lithospheric plates causing geologic activity – (mountain building, volcanic eruptions and earthquakes)

Convection Currents Upper Mantle - COOLER Lower Mantle - HOTTER The magma in the

Convection Currents Upper Mantle - COOLER Lower Mantle - HOTTER The magma in the lower mantle is warmer. It expands, becomes less dense and rises. When it reaches the upper mantle it cools, contracts, becoming more dense and sinks. This constant rise and fall of magma causes the convection currents that drive plate tectonics. The crust plates ride along on top of these convection currents.

Convection Current clip https: //youtu. be/ryr. XAGY 1 dm. E

Convection Current clip https: //youtu. be/ryr. XAGY 1 dm. E

 • The plates have boundaries • As they move they affect one another.

• The plates have boundaries • As they move they affect one another. Convergent Boundary Divergent Boundary Transform Boundary

Plate Tectonics Reference Table You need to know how to read this table!!

Plate Tectonics Reference Table You need to know how to read this table!!

Pacific Plate – Where the Action is! RING OF FIRE!!

Pacific Plate – Where the Action is! RING OF FIRE!!

Hawaii is a chain of islands made from an underwater volcano. Yet Hawaii is

Hawaii is a chain of islands made from an underwater volcano. Yet Hawaii is NOT on a plate boundary. How was Hawaii created?

Hawaiian Hot Spot • Hawaii is in the middle of the Pacific Plate •

Hawaiian Hot Spot • Hawaii is in the middle of the Pacific Plate • Not on a boundary.

Magma Rises under Hawaii • Hot spot is located in the mantle and does

Magma Rises under Hawaii • Hot spot is located in the mantle and does not move • The Pacific Plate moves NW over the hot spot forming a line of volcanoes.

Plate Boundaries!! Divergent Convergent Transform

Plate Boundaries!! Divergent Convergent Transform

Divergent Boundary • When Plates Divide or Separate

Divergent Boundary • When Plates Divide or Separate

Step 1 – Rift Valley • Magma pushes up cracks in the crust •

Step 1 – Rift Valley • Magma pushes up cracks in the crust • Convection causes the separated plates to move and form a rift valley.

Step 2 – Add Water • The valley widens and begins to be filled

Step 2 – Add Water • The valley widens and begins to be filled with water. (Red Sea)

Step 3 – Ocean Formed • Eventually an ocean forms – At the rate

Step 3 – Ocean Formed • Eventually an ocean forms – At the rate of 6 cm per year Ex. Mid Atlantic Ridge

Divergent Boundaries Map

Divergent Boundaries Map

Transform Boundary • Two Plates slide past each other • Also called strike-slip boundary

Transform Boundary • Two Plates slide past each other • Also called strike-slip boundary • Ex: San Andreas Fault in California

San Andreas Fault • The Pacific Plate moves North • The North American Plate

San Andreas Fault • The Pacific Plate moves North • The North American Plate moves South

San Andreas Fault • Causes stress that leads to Earthquakes in California

San Andreas Fault • Causes stress that leads to Earthquakes in California

Convergent Boundaries • 2 Plates colliding into each other. • Example: Himalayan Mountains formed

Convergent Boundaries • 2 Plates colliding into each other. • Example: Himalayan Mountains formed when India collided with Asia

 • We will Continue these notes next class!!! There is a lot to

• We will Continue these notes next class!!! There is a lot to know about Convergent Boundaries!

Questions to answer • What happens along divergent boundaries? 1. 2. • What happen

Questions to answer • What happens along divergent boundaries? 1. 2. • What happen along transform boundaries? 1. 2.