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Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere.

Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

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Page 1: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Plate Tectonics

Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere.

Page 2: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Plate Tectonics

The Earth’s crust is divided into 12 major plates which are moved in various directions.

This plate motion causes them to collide, pull apart, or scrape against each other.

Each type of interaction causes a characteristic set of Earth structures or “tectonic” features.

Refers to the deformation of the crust because of plate interaction

Page 3: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

World Plates

Page 4: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

What Lies Beneath the Tectonic Plates?Below the lithosphere (which makes up the tectonic plates) is the asthenosphere.

Page 5: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Plate Movement

“Plates” of lithosphere are moved around by the underlying hot mantle convection cells

Page 6: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

PLATE TECTONICS VIDEOS

Page 7: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Supercontinents

Alfred Wegener (1912) introduced theory

Pangaea (“all earth”)

Evidence that supercontinent existed Fossil, puzzle-like features, mountain

ranges

Page 8: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

If you look at a map of the world, you may notice that some of the continents could fit together like pieces of a puzzle.

Page 9: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere
Page 10: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Exploring Tectonic Plate Movement

Food Lab

Page 11: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

What Happens at Tectonic Plate Boundaries?

Page 12: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Divergent

Convergent

Transform

Types of Plate Movement

Page 13: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Spreading ridges

As plates move apart new material is erupted to fill the gap

Divergent Boundaries

Page 14: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Age of Oceanic Crust

Courtesy of www.ngdc.noaa.gov

Page 15: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Iceland has a divergent plate boundary running through its middle

Mid Atlantic Ridge

Iceland: An example of continental rifting

Page 16: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Three styles of convergent plate boundaries

Continent-continent collision

Continent-oceanic crust collision

Ocean-ocean collision

Convergent Boundaries

Page 17: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Forms mountains, e.g. European Alps, Himalayas

Continent-Continent Collision

Page 18: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Himalayas

Page 19: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Called SUBDUCTION

Continent-Oceanic Crust Collision

Page 20: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Oceanic lithosphere subducts underneath the continental lithosphere

Oceanic lithosphere heats and dehydrates as it subsides

The melt rises forming volcanism

E.g. The Andes

Subduction

Page 21: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

When two oceanic plates collide, one runs over the other which causes it to sink into the mantle forming a subduction zone.

The subducting plate is bent downward to form a very deep depression in the ocean floor called a trench.

The worlds deepest parts of the ocean are found along trenches.

Mariana Trench

Ocean-Ocean Plate Collision

Page 22: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere
Page 23: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere

Where plates slide past each other

Transform Boundaries

San Andreas Fault

Page 24: Plate Tectonics Students will be able to describe how the lands and oceans are influenced by the flow of energy through the lithosphere