continental drift &plate tectonics whitney isbell for use with my 8 th grade science class 2013

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Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class http://www.middleschoolscience.com 2013

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Page 1: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Continental Drift &Plate Tectonics

Whitney Isbell for use with my 8th Grade Science Class http://www.middleschoolscience.com 2013

Page 2: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Earth’s LayersThe Earth's solid rocky outer crust formed 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: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

The Crust

• Lithosphere is made up of the crust and the upper mantle. The lithosphere makes up the plates that move on top of the Asthenosphere.

Page 4: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

The Mantle

• Layer of Earth between the crust and the core

• Contains most of the Earth’s mass

• A think liquid like silly putty

• Molten rock

Page 5: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

The Core

• Below the mantle and to the center of the Earth

• Outer Core is molten metal

• Inner Core is solid metal

Page 6: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Continental Drift

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

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

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

Shape of the continents fit together like puzzle pieces

Rocks are found in different continents that are the same composition

Called this supercontinent Pangea, Greek for “all Earth”

245 Million years ago

Could not explain why the plates moved

Page 7: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Evidence of Pangea

Page 8: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Tectonic PlatesIn the 1960’s scientists discovered seafloor spreading and convection of the mantle caused the plates to move.

This was the beginning of the theory of plate tectonics

Convection: Heat rises and cool things sink due to density. Magma (molten rock) that is close to the outer core is hotter and begins to rise. As the magma (molten rock) gets closer to the crust it begins to lose heat and sink back down towards the core. This creates convections currents which cause the plates to move.

Page 9: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

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 10: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Sea Floor Spreading

Page 11: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Sea Floor Spreading• Mid Ocean Ridges –

underwater mountain chains; largest is the Mid-Atlantic Ridge where the Atlantic ocean is pulling apart and new land is being formed.

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

• Older Crust is pushedfarther away from the ridge

Page 12: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

How Plates Move

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

Convection Currents

Page 13: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Different Types of Boundaries

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

Page 14: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Divergent Boundary – Arabian and African Plates

Page 15: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Divergent Boundary – Iceland

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

Page 16: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Divergent Boundary – OceanicMid Ocean Ridges

http://www.geology.com

Page 17: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

You can see the Mid-Atlantic Ridge from

space

Magma rises to the surface when plates are pulling apart and form new land

Page 18: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Divergent Boundary – ContinentalRift Valleys (Great African Rift Valley)

http://www.geology.com

Page 19: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

New Land was formed in Africa when two plates

were pulling apart

Page 20: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Convergent Boundary – Indian and Eurasian Plates

Page 21: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Convergent Boundary – Oceanic & Continental

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

Oceanic Plates are denser and will subduct (sink) under continental plates. The sinking oceanic plate will form new magma.

Page 22: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Convergent Boundary – Oceanic & Oceanic

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

Because plates are not the same size the larger oceanic plate will subduct under the less dense oceanic plate and form new magma.

Page 23: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Convergent Boundaries - Continental

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

Two continental plates will buckle against each other and from folded mountains.

Page 24: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

Transform Boundary – San Andreas Fault

www.geology.com Two plates that are sliding past each other will create earthquakes and faults.

Page 25: Continental Drift &Plate Tectonics Whitney Isbell for use with my 8 th Grade Science Class  2013

• Fundamental Questions • What was the early theory of continental drift; who

developed it, and when was it developed? • What were the discoveries that led to a theory of plate

tectonics, and when were these discoveries made? • What is Earth's lithosphere made of, and how does it affect

crustal features? • What features of the Earth's crust do convergent, divergent,

and transform boundaries form? • What land features formed by the movement of tectonic

plates can be observed using images from space?