Plate Tectonics 7 th Grade Science. Area of Focus: Plate Tectonics Copyright © 2010 Ryan P. Murphy

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Plate Tectonics 7th Grade Science

• Area of Focus: Plate Tectonics

Copyright © 2010 Ryan P. Murphy

• Plate tectonics: The earth’s crust and upper mantle are broken into sections called plates. – These plates float on the mantle like rafts (moving

very slowly)

Copyright © 2010 Ryan P. Murphy

• Plate tectonics: The earth’s crust and upper mantle are broken into sections called plates. – These plates float on the mantle like rafts (moving

very slowly)

Copyright © 2010 Ryan P. Murphy

• Continental Drift: The gradual movement of the continents across the earth.

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• The speed at which the plates move is about the speed at which your fingernails grow.

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• Video! How did the continents form?

• In 1915, The German geologist Alfred Wegener (1880-1930) proposed continental drift.

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• In 1915, The German geologist Alfred Wegener (1880-1930) proposed continental drift.

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“I say.” “Africa and South America fit strangely like two puzzle pieces.”

• In 1915, The German geologist Alfred Wegener (1880-1930) proposed continental drift. Not accepted until the 1950’s!

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• Evidence for continental drift.– -– -– -– - – -

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• The shapes match.

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• Same fossils found on different continents– These are the pictures on the puzzle pieces.

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• Same fossils found on different continents– These are the pictures on the puzzle pieces.

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• The Same rock structures on different continents

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• What is this a fossil of?– Where would you expect to find a specimen like

this on the planet?

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• Answer! This is a fossilized tropical plant found on Antarctica.

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• Answer! This is a fossilized tropical plant found on Antarctica.– Remember, the continents have moved and

Antarctica use to be in a warmer climate.

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• Fossils of plants and animals in Antarctica

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• Behold the Supercontinent! Pangea

?

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• Behold the Supercontinent! Pangea

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• Pangea: The “Super Continent” – All of the plates were once together.

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• Pangea: The “Super Continent” – All of the plates were once together.

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– Gondwondaland and Laurasia were two mega continents after Pangea.

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• Current Day + or – 4mm

• What causes continental drift and plate tectonics?

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• Answer! – Convection currents (Remember heat rises) move

the plates

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• Answer! – Convection currents (Remember heat rises) move

the plates

Copyright © 2010 Ryan P. Murphy

• Answer! – Convection currents (Remember heat rises) move

the plates

Copyright © 2010 Ryan P. Murphy

• Answer! – Convection currents (Remember heat rises) move

the plates

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Video! Plate Tectonics

• Layers of the earth

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• Layers of the earth

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• Layers of the earth

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• Layers of the earth

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• Layers of the earth

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• Layers of the earth

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• Earth’s layers formed early in it’s long history.

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• Earth’s layers formed early in it’s long history.– (Archean Eon) Gravity pulled heavy elements

toward the middle.

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• Inner Core: Solid Iron and Nickel (Dense).

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Hot and Dense

Less Hot and Dense

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• The spinning inner cores of solid and liquid Iron creates a giant electromagnetic field.

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• Outer Core: Liquid Iron and Nickel

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• Mantle: Composed of Magnesium Silicates, Iron, Calcium

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• Mantle: Composed of Magnesium Silicates, Iron, Calcium

- Outer Mantle (Asthenosphere)

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• Mantle: Composed of Magnesium Silicates, Iron, Calcium

- Outer Mantle (Asthenosphere)- Lithosphere (Crust)

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• Review! Heat from the earth rises and run along plates causing them to move.

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• New Area of Focus: Earth’s Plate Boundaries.

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• Two types of Crust– -– -

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• Oceanic Crust: More dense so it sinks more (Basalts).

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• Continental Crust: Less Dense so it floats higher (Granites)

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• Which plates below are ocean plates?

• Answer! Nazca Plate.

• Answer! Pacific Plate

• Answer!

• Answer!

• Activity! Using Google Earth to look at divergent ocean plate boundaries on the sea floor.– http://www.google.com/earth/index.html

• Divergent Boundaries: Crust is created as two or more plates pull away from each other.

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Newer Newer

Newer NewerOlder Older

Newer NewerOlder Older

Newer NewerOlder Older

4 miles thick

• Convergent Boundaries: Crust is destroyed and recycled back into the interior of the earth.– One plate dives under another.

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• Convergent Boundaries: Crust is destroyed and recycled back into the interior of the earth.– One plate dives under another.

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• Ocean vs. Continent (Subduction zone)

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• Ocean vs. Continent (Subduction zone)– The oceanic plate is forced below the continental

plate.

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• What is the “Ring of Fire”?

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• What is the “Ring of Fire”?

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• Ring of Fire: A zone of frequent earthquakes and volcanic eruptions that encircles the basin of the Pacific Ocean.

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• Ring of Fire: A zone of frequent earthquakes and volcanic eruptions that encircles the basin of the Pacific Ocean.

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• Ring of Fire: A zone of frequent earthquakes and volcanic eruptions that encircles the basin of the Pacific Ocean.

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• Many tropical Islands like this are created by ocean plates and volcanism.

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Ocean Plate

Ocean Plate

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Ocean Plate

Ocean Plate

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Ocean Plate

Ocean Plate

Volcanic Arch Island Chain / Archipelago

• Video Link! New volcanic island forming– http://www.youtube.com/watch?v=kwETZSARMg

E

• Transform-Fault Boundaries: Where two plates are sliding horizontally past one another.

Copyright © 2010 Ryan P. Murphy

• Coastal California and the Baja Peninsula will become an Island.

• Coastal California and the Baja Peninsula will become an Island.

• Coastal California and the Baja Peninsula will become an Island.

• Continental Convergence: (Mountain Building).

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• The Swiss Alps is an example of mountains that form when continents collide.– The African Plate is colliding with the European Plate

• The Swiss Alps is an example of mountains that form when continents collide.– The African Plate is colliding with the Eurasian plate/

• Indian Continental Plate is crashing into Asian Plate causing the mountains to form. – They are still growing.

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• Himalayas: Tallest Mountains on Earth.

• Continent Divergence (Moving apart).

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• Ocean vs. Ocean Convergence

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• Antilles in Caribbean

• Aleutian Islands Alaska

• Indonesia – Every triangle is a volcano

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