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

Dec 13, 2015

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Page 1: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

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

http://www.middleschoolscience.com 2009

Page 2: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

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 Liz LaRosa for use with my 5 th Grade Science Class  2009 .

The Crust

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

Page 4: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

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 Liz LaRosa for use with my 5 th Grade Science Class  2009 .

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 Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Tectonic Plates

Page 7: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

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 8: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

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 9: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Evidence of Pangea

Page 10: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Sea Floor Spreading

Page 11: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

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 Liz LaRosa for use with my 5 th Grade Science Class  2009 .

How Plates Move

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

Page 13: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Bell work p.20

What is the name of the place where two plates meet?

Content Goal:To be able to explain the three types of plate boundaries.

Page 14: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

2/5 BELL WORK

1. Take out a piece of notebook paper.2. Put your full name and period in top right

corner.3. Number your paper 1-34. Skip a line, add number 45. Skip 3 lines, add number 56. You will have ten minutes to complete pop

quiz

Page 15: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Different Types of Boundaries

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

Page 16: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Divergent Plate Boundaries

• Plates separate• Usually on ocean floor• New rocks formed• Called rift valley• Examples: Mid-Atlantic Ridge, Iceland (above

sea level)

Page 17: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Divergent Boundary – Iceland

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

Page 18: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Iceland rift valley

Page 19: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Progression of Rift Valleys

Page 20: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Divergent Boundary – OceanicSea Floor Spreading

http://www.geology.com

Page 21: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Divergent Boundary - Continental

http://www.geology.com

Page 22: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Divergent Boundary – Arabian and African Plates

Page 23: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

AFRICAN RIFT VALLEY

Page 24: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .
Page 25: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Convergent Plate BoundariesOcean-Continental

• More dense plate subducts when plates converge

• Oceanic crust subducts under continental plate

• Forms volcanic mountain chains to east of subduction

• Deep earthquakes to the west of subduction

Page 26: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Convergent Boundary – Oceanic & Continental

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

Page 27: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Mt Ranier and Crator Lake

Page 28: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Oceanic-Oceanic Convergent Plate Boundaries

• More dense plate subducts• Forms a deep open trench to west of subduction

zone• Island arcs form 300km to east of subduction

zone

Page 29: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Convergent Boundary – Oceanic & Oceanic

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

Page 30: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Aleutian Islands in Alaska/Japan/Phillipines

Page 31: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Continental-Continental Convergent Boundaries

• More dense plate subducts, often both plates are of same density

• Major mountain ranges form

Page 32: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Convergent Boundaries - Continental

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

Page 33: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Great Smoky Mountains/Appalachian

Mountains/Rocky Mountains

Page 34: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Convergent Boundary – Indian and Eurasian PlatesHimalayan Mountain Range - Mt. Everest

Page 35: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Hot Spots

Page 36: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

Transform Boundary – San Andreas Fault

www.geology.com

Page 37: Plate Tectonics Liz LaRosa for use with my 5 th Grade Science Class  2009 .

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