Download - DO NOW

Transcript
Page 1: DO NOW

DO NOW

• Take out last night’s homework – Continental Drift vs. Sea-Floor Spreading handout

• Turn to your neighbor and share your answers with your neighbor.

Page 2: DO NOW

PLATE TECTONICS

Page 3: DO NOW

Plate Tectonics• The idea that Earth’s surface is broken into

plates that slide slowly across the mantle• Mantle- the layer beneath the Earth’s crust

Page 4: DO NOW

Tectonic Plates

Page 5: DO NOW

Tectonic Plates

Page 6: DO NOW

What causes the plates to move?• Convection currents caused by magma

Page 7: DO NOW

The Lithosphere and Asthenosphere

• The crust and the layer of the upper mantle that form plates are called the lithosphere

• They rest on the upper mantle called the asthenosphere

• Earth has two kinds of crust: continental crust and oceanic crust– Continents are made of continental

crust, which is made up of rocks that are less dense than oceanic crust

– The ocean floor is made up of oceanic crust, which is made up of rocks that are more dense than continental crust

Page 8: DO NOW

What is a plate boundary?

• Plate boundaries are where the edges of plates meet

• There are three types of plate boundaries• The type of boundary depends on whether

the plates are moving toward each other, separating, or sliding past each other

Page 9: DO NOW

Three Types of Plate Boundaries

Page 10: DO NOW

Plate Boundaries

Page 11: DO NOW

Divergent Boundaries

• Divergent boundary- form where plates diverge, or move away from each other

- These boundaries are under oceans and build undersea mountain ranges called mid-ocean ridges

Page 12: DO NOW

Divergent Boundaries

Page 13: DO NOW

Convergent Boundaries

• Convergent boundary- form where plates collide -The pressure and violence at

convergent boundaries produces mountains, bands of volcanic activity, and deep ocean trenches

Page 14: DO NOW

Convergent Boundaries• Oceanic and Continental Crust Convergent

Boundary

Page 15: DO NOW

Convergent Boundaries• Continental and Continental Crust Convergent

Boundary

Page 16: DO NOW

Convergent Boundaries• Oceanic and Oceanic Crust Convergent Boundary

Page 17: DO NOW

Transform Fault Boundaries

• Transform fault boundary- form where two plates slide past each other - As plates smash and grind past

each other, there are many earthquakes

Page 18: DO NOW

Transform Fault Boundaries


Top Related