The asthenosphere consists of solid rock that is

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The asthenosphere consists of solid rock that is flowing. But it’s not all flowing

The asthenosphere consists of solid rock that is flowing. But it’s not all flowing in the same direction.

Theory of Plate Tectonics • Theory that pieces of lithosphere move around on top

Theory of Plate Tectonics • Theory that pieces of lithosphere move around on top of the asthenosphere

Plate Boundaries • The edges of different pieces of The lithosphere meet at lines

Plate Boundaries • The edges of different pieces of The lithosphere meet at lines called plate boundaries

Plate Boundaries Plate Videos

Plate Boundaries Plate Videos

So the plates move. Now What? • As the plates move, they produce changes

So the plates move. Now What? • As the plates move, they produce changes in Earth’s surface, including volcanoes, earthquakes, mountain ranges, and deepocean trenches.

3 Types of Plate Boundaries Divergent Convergent Transform Divergent

3 Types of Plate Boundaries Divergent Convergent Transform Divergent

3 Types of Boundaries Divergent boundary= two plates move apart • Magma rises and

3 Types of Boundaries Divergent boundary= two plates move apart • Magma rises and creates new crust or seafloor Causes: midocean ridges, rift valleys, new crust , volcanoes

Divergent Boundaries © All Rights Reserved. Diverging Africa

Divergent Boundaries © All Rights Reserved. Diverging Africa

Diverging Iceland

Diverging Iceland

3 Types of Boundaries • Convergent= when two tectonic plates push into one another.

3 Types of Boundaries • Convergent= when two tectonic plates push into one another.

Convergent Boundaries • Continental vs. Continental • Continental vs. Oceanic • Oceanic vs. Oceanic

Convergent Boundaries • Continental vs. Continental • Continental vs. Oceanic • Oceanic vs. Oceanic

Continental vs. Continental • When two continental crustal plates collide, the continents buckle upward

Continental vs. Continental • When two continental crustal plates collide, the continents buckle upward and form mountains. Himalayas- Asia

Himalayas- Asia

Himalayas- Asia

Oceanic vs. Continental • The oceanic plate slides under the continental plate. • The

Oceanic vs. Continental • The oceanic plate slides under the continental plate. • The continental crust crumbles and forms new mountains.

Oceanic vs. Continental • Ex: Andes mtn in S. America Cascade Mtns. in N.

Oceanic vs. Continental • Ex: Andes mtn in S. America Cascade Mtns. in N. America- Mt. St. Helens

Oceanic vs. Oceanic • Two oceanic plates collide, one of the oceanic plates slides

Oceanic vs. Oceanic • Two oceanic plates collide, one of the oceanic plates slides under the other. • also called a subduction zone

Oceanic vs. Oceanic Hawaiian Islands

Oceanic vs. Oceanic Hawaiian Islands

Transform boundary • When two tectonic plates slide past each other horizontally Produces? Earthquakes

Transform boundary • When two tectonic plates slide past each other horizontally Produces? Earthquakes

San Andreas Fault

San Andreas Fault

New Madrid Fault

New Madrid Fault

Examples of Convection DOS • Convection example • Convection in a room

Examples of Convection DOS • Convection example • Convection in a room

How do the plates move? • CONVECTION CURRENTS • Hot material rises while cooler

How do the plates move? • CONVECTION CURRENTS • Hot material rises while cooler material near the surface sinks

How do the plates move? • CONVECTION CURRENTS • Hot material from deep within

How do the plates move? • CONVECTION CURRENTS • Hot material from deep within the Earth rises while cooler material near the surface sinks • http: //education. sdsc. edu/optiputer/flash/convection. htm

Convection currents

Convection currents

How do we know? • Sea-floor spreading =new ocean floor is created as two

How do we know? • Sea-floor spreading =new ocean floor is created as two lithospheric plates pull away from one another. Sea-floor spreading

Seafloor spreading

Seafloor spreading

The Plates Move… So what now? Which way? • 50 million years

The Plates Move… So what now? Which way? • 50 million years