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Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class http://www.middleschoolscience.com 2009

Plate Tectonics

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Plate Tectonics. Liz LaRosa for use with my 5 th Grade Science Class http://www.middleschoolscience.com 2009 . Earth’s Layers. The Earth's rocky outer crust solidified billions of years ago, soon after the Earth formed. - PowerPoint PPT Presentation

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Page 1: Plate Tectonics

Plate TectonicsLiz LaRosa for use with my 5th Grade Science Class

http://www.middleschoolscience.com 2009

Page 2: Plate Tectonics

Earth’s LayersThe Earth's rocky outer crust solidified billions of years ago, soon after the Earth formed.

This crust is not a solid shell; it is broken up into huge, thick plates that drift atop the soft, underlying mantle.

Page 3: Plate Tectonics

The Crust

• Outermost layer• 5 – 100 km thick• Made of Oxygen, Silicon, Aluminum

Page 4: Plate Tectonics

The Mantle• Layer of Earth between

the crust and the core• Contains most of the

Earth’s mass• Has more magnesium

and less aluminum and silicon than the crust

• Is denser than the crust

Page 5: Plate Tectonics

The Core• Below the mantle

and to the center of the Earth

• Believed to be mostly Iron, smaller amounts of Nickel, almost no Oxygen, Silicon, Aluminum, or Magnesium

Page 6: Plate Tectonics

Tectonic Plates

Page 7: Plate Tectonics

Plate Tectonics

• Greek – “tektonikos” of a builder• Pieces of the lithosphere(Earth’s crust) that

move around• Each plate has a name• Fit together like jigsaw puzzles• Float on top of mantle similar to ice cubes

in a bowl of water

Page 8: Plate Tectonics

Continental Drift

http://members.enchantedlearning.com/subjects/astronomy/planets/earth/Continents.shtml

Alfred Wegener 1900’s theory that Continents were once a single land mass that drifted apart.

Fossils of the same plants and animals are found on different continents

Called this supercontinent Pangaea, Greek for “all Earth”

245 Million years ago

Split again – Laurasia & Gondwana 180 million years ago

Page 9: Plate Tectonics

Evidence of Pangea

Page 10: Plate Tectonics

Sea Floor Spreading

Page 11: Plate Tectonics

Sea Floor Spreading

• Mid Ocean Ridges – underwater mountain chains that run through the Earth’s Basins

• Magma rises to the surface and solidifies and new crust forms

• Older Crust is pushedfarther away from the ridge

Page 12: Plate Tectonics

How Plates Move

http://pubs.usgs.gov/gip/dynamic/unanswered.html

Page 13: Plate Tectonics

Different Types of Boundaries

http://pubs.usgs.gov/gip/dynamic/understanding.html

Page 14: Plate Tectonics

Divergent Boundary – Arabian and African Plates

Arabian Plate

African PlateRed Sea

Page 15: Plate Tectonics

Divergent Boundary – Iceland

http://pubs.usgs.gov/gip/dynamic/understanding.html

Page 16: Plate Tectonics

Divergent Boundary - Oceanic

http://www.geology.com

Page 17: Plate Tectonics

Divergent Boundary - Continental

http://www.geology.com

Page 18: Plate Tectonics

Convergent Boundary – Indian and Eurasian PlatesThe red marker identifies the Himalaya Mountains

Indian Plate

Eurasian Plate

Page 19: Plate Tectonics

Convergent Boundary – Oceanic & Continental

http://pubs.usgs.gov/gip/dynamic/understanding.html & http://www.geology.com

Page 20: Plate Tectonics

Convergent Boundary – Oceanic & Oceanic

http://pubs.usgs.gov/gip/dynamic/understanding.html & http://www.geology.com

NOTE – PLATES ARE REVERSED

Page 21: Plate Tectonics

Convergent Boundaries - Continental

http://pubs.usgs.gov/gip/dynamic/understanding.html & http://www.geology.com

Page 22: Plate Tectonics

Transform Boundary – San Andreas Fault

www.geology.com

Page 23: Plate Tectonics

Review

• Name the 3 main layers of the Earth• What is a tectonic plate?• What was Pangea?• What is Sea-Floor spreading?• Name the three different types of plate

boundaries and one location on Earth for each one