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Plate tectonics

Plate tectonics

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Plate tectonics. Tectonic Plates. Plate Tectonics. Greek – “tektonikos” of a builder Pieces of the lithosphere 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. Continental Drift. Alfred Wegener 1900’s - PowerPoint PPT Presentation

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Page 1: Plate tectonics

Plate tectonics

Page 2: Plate tectonics

Tectonic Plates

Page 3: Plate tectonics

Plate Tectonics

• Greek – “tektonikos” of a builder• Pieces of the lithosphere 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 4: Plate tectonics

Continental Drift

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

Alfred Wegener 1900’sContinents were once a single land mass that drifted apart.

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

Called this supercontinent Pangea, Greek for “all Earth”

245 Million years ago

Split again – Laurasia & Gondwana 180 million years ago

Page 5: Plate tectonics

Evidence of Pangea

Page 6: Plate tectonics

Sea Floor Spreading

Page 7: 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 8: Plate tectonics

Why do plates move?

Page 9: Plate tectonics

Convection currents

Page 10: Plate tectonics

Convection currents• What are they?• How do they make plates move?• When mantle rocks near the radioactive core are heated, they

become less dense than the cooler, upper mantle rocks. These warmer rocks rise while the cooler rocks sink, creating slow, vertical currents within the mantle (these convection currents move mantle rocks only a few centimeters a year). This movement of warmer and cooler mantle rocks, in turn, creates pockets of circulation within the mantle called convection cells. The circulation of these convection cells could very well be the driving force behind the movement of tectonic plates over the athenosphere.

Page 11: Plate tectonics

Subduction

• What is it?• One plate sinks underneath the other because

it is more dense.

Page 12: Plate tectonics

How Plates Move

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

Page 13: Plate tectonics

Convection currents

Page 14: Plate tectonics

• Destructive vs. Constructive forces• Define both of the terms below:• Constructive forces- builds the Earth up• Destructive forces- Breaks the Earth down

Page 15: Plate tectonics

Destructive or constructive?type destructive constructive both

Erosion

Weathering

Deposition

Volcano

earthquake

Page 16: Plate tectonics

Different Types of Boundaries

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

Page 17: Plate tectonics

Plate boundaries

• Transform• Plates slide past each other• Earthquakes form

Page 18: Plate tectonics

Transform Boundary – San Andreas Fault

www.geology.com

Page 19: Plate tectonics

Plate boundaries

• Divergent• Plates divide• In ocean- will be mid-ocean ridges• On land- rift valleys• Why? As plates spread apart, magma rises

through the gap and forms new crust

Page 20: Plate tectonics

Divergent Boundary – Arabian and African Plates

Arabian Plate

African PlateRed Sea

Page 21: Plate tectonics

Divergent Boundary – Iceland

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

Page 22: Plate tectonics

Divergent Boundary - Oceanic

http://www.geology.com

Page 23: Plate tectonics

Divergent Boundary - Continental

http://www.geology.com

Page 24: Plate tectonics

Convergent Boundary – Indian and Eurasian Plates

Indian Plate

Eurasian Plate

Page 25: Plate tectonics

Convergent Boundary – Oceanic & Continental

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

Page 26: Plate tectonics

Plate boundaries

• Convergent• Plates collide (go together)• When ocean plates meet continent plates, an

ocean trench forms with volcano on the land• Why? Ocean plate is more dense than

continental and sinks under it into mantle (subduction)

Page 27: Plate tectonics

Convergent Boundary – Oceanic & Oceanic

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

NOTE – PLATES ARE REVERSED

Page 28: Plate tectonics

Plate boundaries

• Convergent• Plates collide (go together)• When ocean plates meet ocean plates, an

ocean trench forms with magma forming islands

• Why? The ocean plate that is more dense will sink under the other (subduction)

Page 29: Plate tectonics

Convergent Boundaries - Continental

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

Page 30: Plate tectonics

Plate boundaries

• Convergent• Plates collide (go together)• When continent plates meet continent plates, mountains form Why? Continental plates buckle up as they

push together

Page 31: Plate tectonics

Plate tectonic animations

• http://www.nature.nps.gov/geology/usgsnps/animate/pltecan.html

Page 32: Plate tectonics

Additional activities:

• Plate tectonics www.brainpop.com• Volcanoes

http://www.brainpop.com/science/earthsystem/volcanoes/

• Earthquake http://www.brainpop.com/science/earthsystem/earthquakes/

• Pangaea activity worksheet• Plate boundary prediction worksheet