continental drift and plate tectonics

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Geography of Canada Continental Drift and Plate Tectonics http://www.youtube.com/watch?v=_5q8hzF9VVE 11:56mins

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Continental Drift and Plate Tectonics. Geography of Canada. http://www.youtube.com/watch?v=_5q8hzF9VVE 11:56mins. Earth’s Interior. HYDROSPHERE. ATMOSPHERE. Air. Water. Crust - 8-64 km thick - cold - Granite and Basalt. Land. LITHOSPHERE. Mantle - 1800 km thick - PowerPoint PPT Presentation

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Page 1: Continental Drift and  Plate Tectonics

Geography of Canada

Continental Drift and

Plate Tectonicshttp://www.youtube.com/watch?v=_5q8hzF9VVE 11:56mins

Page 2: Continental Drift and  Plate Tectonics

Earth’s Interior

Crust- 8-64 km thick- cold- Granite and Basalt

Mantle- 1800 km thick- hot, liquid rock- Magnesium and Silicon

Outer Core- 2000 km thick- 3 - 4000°C- liquid Nickel and Iron

Inner Core- 1400 km thick- 5 - 6000°C- solid Nickel and Iron

Air

Land

Water

LITHOSPHERE

HYDROSPHERE ATMOSPHERE

Page 3: Continental Drift and  Plate Tectonics

Theory of Continental Drift

• Alfred Wegener, in 1915, came up with the idea of Continental Drift.

• He said that the continents of the Earth slowly moved. He said they used to be one big continent (pangaea) a long time ago, but split apart and moved to where they are today.

Page 4: Continental Drift and  Plate Tectonics

Plate Tectonics - Continental Drift

Page 5: Continental Drift and  Plate Tectonics

Continental Drift

Page 6: Continental Drift and  Plate Tectonics

http://eesc.ldeo.columbia.edu/courses/w4947/images/plate_motions.gif

Page 7: Continental Drift and  Plate Tectonics

Plate Tectonics - Continental Drift

Antarctica

THE CONTINENTS TODAY

Page 8: Continental Drift and  Plate Tectonics

Wegener’s Proof

3 pieces of evidence for his theory (idea) were:

1. Rocks that were the same age and type

2. The shape of the continents (look like puzzle pieces that fit together)

3. Fossils that were the same

Page 9: Continental Drift and  Plate Tectonics

Plate Tectonics - Continental Drift

PROOF!

Page 10: Continental Drift and  Plate Tectonics

Theory of Plate Tectonics

• This theory (idea) was made by J. Tuzo Wilson in 1968.

• He said that the Earth’s crust is made up of many plates and that these plates move on top of the mantle. The movement of the plates causes changes to the Earth’s surface.

Page 11: Continental Drift and  Plate Tectonics

• Crust eventually broke apart into pieces called PLATES

• The plates float on the interior of the earth, like crackers on a bowl of hot soup

Page 12: Continental Drift and  Plate Tectonics

Plate Tectonics cntd.

• The Earth’s crust is divided into 12 major plates.• Heat from deep inside the earth causes plates to

move • Earth’s continents sit on plates, so when the

plates move, the continents move with them• The movement of these plates is called PLATE

TECTONICS

Page 13: Continental Drift and  Plate Tectonics

• On average, the plates move about as fast as fingernails grow…an inch or so every year

Page 14: Continental Drift and  Plate Tectonics

The Plates

Plates are pieces of the Earth’s crust.

• The plates that move are both continental and ocean plates.

Page 15: Continental Drift and  Plate Tectonics

Plate Tectonics Cntd.

• Plates move constantly, and when they move different things happen…

• They can collide, pull apart, or scrape against each other.

• Each type of movement causes changes on Earth’s surface… structures or “tectonic” features (ex. Mountains, volcanoes).

• The word, tectonic, refers to the distorting of the crust as result of plate interaction.

Page 16: Continental Drift and  Plate Tectonics

Plate Tectonics Map

Page 17: Continental Drift and  Plate Tectonics

Convection Currents

• Plates move because of Convection Currents

– The mantle is made of much denser, thicker material, because of this the plates "float" on it like oil floats on water.

– Movement of plates is caused by very hot material at the deepest part of the mantle rising, then cooling, sinking again and then heating, rising and repeating the cycle over and over

Page 18: Continental Drift and  Plate Tectonics

Convection Currents