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Plate Tectonics Plate Tectonics

Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

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Page 1: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Plate TectonicsPlate Tectonics

Page 2: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

© 2011 Pearson Education, Ic.

Global Plate BoundariesGlobal Plate Boundaries

Page 3: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries
Page 4: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Plate BoundariesPlate Boundaries

►There are 3 main There are 3 main plate boundaries:plate boundaries:

► 1) Convergent 1) Convergent BoundaryBoundary

► 2) Divergent 2) Divergent BoundaryBoundary

► 3) Transform 3) Transform BoundaryBoundary

Page 5: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Types of Plate BoundariesTypes of Plate Boundaries

Page 6: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Draw With Me Draw With Me

Page 7: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

1. Convergent 1. Convergent BoundariesBoundaries

►Occurs when 2 Occurs when 2 plates plates collide.collide.

Oceanic plate is Oceanic plate is denser (3.2 g/cmdenser (3.2 g/cm33), ), faster and thinner - it faster and thinner - it is usually forced is usually forced under the under the continental plate continental plate (2.8 g/cm(2.8 g/cm33).).

Page 8: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

The rock in the Oceanic plate melts as the The rock in the Oceanic plate melts as the plate sinks. The melted rock rises up plate sinks. The melted rock rises up causing volcanic eruptions.causing volcanic eruptions.

► The area of convergence is called a The area of convergence is called a SUBDUCTION ZONESUBDUCTION ZONE. .

► When two continental plates collide:When two continental plates collide: They are the same density. They are the same density. This causes the plates to fold and bend This causes the plates to fold and bend

(mountain building) as well as earthquakes.(mountain building) as well as earthquakes.

Page 9: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries
Page 10: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Convergent Boundary Convergent Boundary

► Plates move toward each otherPlates move toward each other► Oceanic crust destroyedOceanic crust destroyed

Ocean trenchOcean trench Volcanic arcVolcanic arc

Page 11: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Example of a Convergent Example of a Convergent Plate BoundaryPlate Boundary

► South America: South America: ► Oceanic Nazca Plate is Oceanic Nazca Plate is

colliding into the South colliding into the South America plate. America plate.

► Producing the Andes Producing the Andes Mountains (volcanoes Mountains (volcanoes along the mountain crest) along the mountain crest) and formed a deep trench and formed a deep trench off the coast in the Pacific off the coast in the Pacific Ocean. Ocean.

http://http://earthguide.ucsd.edu/eoc/earthguide.ucsd.edu/eoc/teachers/t_tectonics/teachers/t_tectonics/p_subduction.htmlp_subduction.html

Page 12: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries
Page 13: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

© 2011 Pearson Education, Inc.

Page 14: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Convergent BoundariesConvergent Boundaries

Page 15: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Let’s do some drawing!Let’s do some drawing!

Page 16: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Divergent Plate BoundariesDivergent Plate Boundaries► Plates are being Plates are being pulled apart pulled apart

by convection currents in the by convection currents in the mantle.mantle.

► As the plates separate along As the plates separate along the boundary, they crack into the boundary, they crack into faults and blocks. Magma faults and blocks. Magma from the mantle rises through from the mantle rises through the cracks. This cools and new the cracks. This cools and new crust is formed along the crust is formed along the boundary.boundary.

► Earthquakes occur along the Earthquakes occur along the faults, and volcanoes form faults, and volcanoes form where the magma reaches the where the magma reaches the surface. surface.

Page 17: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Mid Atlantic RidgeMid Atlantic Ridge

► Mid-Atlantic Ridge is Mid-Atlantic Ridge is a Divergent Plate a Divergent Plate Boundary.Boundary.

► Over 15 000 km long.Over 15 000 km long.► Average height of Average height of

volcanoes - 3 km.volcanoes - 3 km.

► http://http://earthguide.ucsd.edu/earthguide.ucsd.edu/eoc/teachers/eoc/teachers/t_tectonics/t_tectonics/p_seafloorspreading.p_seafloorspreading.htmlhtml

Page 18: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries
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Age of Ocean FloorAge of Ocean Floor

Page 20: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries
Page 21: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Example of a Divergent Plate Example of a Divergent Plate BoundaryBoundary

http://www.wwnorton.com/college/geo/egeo/http://www.wwnorton.com/college/geo/egeo/animations/ch2.htm#1 animations/ch2.htm#1 The Process of RiftingThe Process of Rifting

Page 22: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Divergent Boundary Divergent Boundary

► Plates move apartPlates move apart► Mid-ocean ridgeMid-ocean ridge

Rift valleyRift valley► New ocean floor New ocean floor

createdcreated

Page 23: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Sea Floor DiagramSea Floor Diagram

© 2011 Pearson Education, Inc.

Page 24: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Generation of a Divergent Generation of a Divergent BoundaryBoundary

Page 25: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Types of Spreading CentersTypes of Spreading Centers

Page 26: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Sea Floor SpreadingSea Floor Spreading►Mid-ocean ridge Mid-ocean ridge – spreading center– spreading center►Subduction zones Subduction zones – oceanic trench – oceanic trench

site of crust destructionsite of crust destruction► http://www.watchknowlearn.org/Video.aspx?http://www.watchknowlearn.org/Video.aspx?

VideoID=698&CategoryID=2464VideoID=698&CategoryID=2464

Page 27: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

© 2011 Pearson Education, Inc.

Earthquakes As EvidenceEarthquakes As Evidence

►Earthquake activity mirrors tectonic Earthquake activity mirrors tectonic plate boundaries.plate boundaries.

Page 28: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Global Distribution of Global Distribution of Earthquakes Earthquakes

Page 29: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Transform BoundaryTransform Boundary► Places where plates slide Places where plates slide

past each other sideway.past each other sideway.

► Transform boundaries are Transform boundaries are not marked by spectacular not marked by spectacular surface features, but their surface features, but their sliding motion causes lots of sliding motion causes lots of earthquakesearthquakes..

► The slice of California to the The slice of California to the west of the fault is slowly west of the fault is slowly moving north relative to the moving north relative to the rest of California. rest of California.

Page 30: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

The Problems of Haiti…The Problems of Haiti…

Page 31: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries
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Page 33: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Interactive Plate Tectonic Interactive Plate Tectonic Map Map

►http://geology.com/plate-http://geology.com/plate-tectonics.shtmltectonics.shtml

►Go to the following site and complete Go to the following site and complete the activity!the activity!

Page 34: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries
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Page 36: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries
Page 37: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Earth’s Magnetic FieldEarth’s Magnetic Field

►http://science.howstuffworks.com/http://science.howstuffworks.com/environmental/planet-earth-videos-environmental/planet-earth-videos-playlist.htm#video-29143playlist.htm#video-29143

Page 38: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries
Page 39: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

HOT SPOT VOLCANOES HOT SPOT VOLCANOES

►http://www.wwnorton.com/college/http://www.wwnorton.com/college/geo/egeo/animations/ch2.htm#1 geo/egeo/animations/ch2.htm#1 AnimationAnimation

Page 40: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Examples of Plate BoundariesExamples of Plate Boundaries

Page 41: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Transform Boundary Transform Boundary FeaturesFeatures

► Oceanic Transform Fault Oceanic Transform Fault – ocean floor only– ocean floor only► Continental Transform Fault Continental Transform Fault – cuts across – cuts across

continentcontinent► All transform faults All transform faults

occur between occur between mid-ocean ridge mid-ocean ridge segments.segments.

Page 42: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries
Page 43: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Global Hotspot LocationsGlobal Hotspot Locations

Page 44: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Hawaiian Island – Emperor Hawaiian Island – Emperor Seamount NematathSeamount Nematath

Page 45: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Plate Tectonics FeaturesPlate Tectonics Features► Seamounts Seamounts

Rounded topsRounded tops► Tablemounts Tablemounts oror guyots guyots

Flattened topsFlattened tops► Subsidence of flanks of mid-ocean ridgeSubsidence of flanks of mid-ocean ridge► Wave erosion may flatten seamountWave erosion may flatten seamount

Page 46: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries
Page 47: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Detecting Plate Motion with Detecting Plate Motion with SatellitesSatellites

Page 48: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

World Map 50 million Years in World Map 50 million Years in FutureFuture

Page 49: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Coral Reef DevelopmentCoral Reef Development

► Fringing reefs Fringing reefs – – develop along develop along margin of landmassmargin of landmass

► Barrier reefs Barrier reefs – – separated from separated from landmass by lagoonlandmass by lagoon

► AtollsAtolls – reefs – reefs continue to grow continue to grow after volcanoes are after volcanoes are submergedsubmerged

Page 50: Plate Tectonics. © 2011 Pearson Education, Ic. Global Plate Boundaries

Coral Reef DevelopmentCoral Reef Development