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Naturalists at Large: Plate tectonics

May 16, 2015

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Phat Nattie

Naturalists at Large Plate Tectonics Slide Show
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Page 1: Naturalists at Large: Plate tectonics
Page 2: Naturalists at Large: Plate tectonics

Theory of Plate TectonicsTheory of Plate Tectonics

Plate TectonicsPlate Tectonics

Plate BoundariesPlate Boundaries

Causes of Plate TectonicsCauses of Plate Tectonics

Page 3: Naturalists at Large: Plate tectonics

Plate TectonicsPlate Tectonics

Page 4: Naturalists at Large: Plate tectonics

What is Plate TectonicsWhat is Plate Tectonics

• The Earth’s crust and upper mantle are broken into sections called plates

• Plates move around on top of the mantle like rafts

Page 5: Naturalists at Large: Plate tectonics
Page 6: Naturalists at Large: Plate tectonics

What is the What is the LithosphereLithosphere??

• The crust and part of the upper mantle = lithosphere–100 km thick

–Less dense than the material below it so it “floats”

Page 7: Naturalists at Large: Plate tectonics

What is the What is the AsthenoshereAsthenoshere??

• The plastic layer below the lithosphere = asthenosphere

• The plates of the lithosphere float on the asthenosphere

Page 8: Naturalists at Large: Plate tectonics
Page 9: Naturalists at Large: Plate tectonics

2 Types of Plates2 Types of Plates

• Ocean plates - plates below the oceans

• Continental plates - plates below the continents

Page 10: Naturalists at Large: Plate tectonics

Plate BoundariesPlate Boundaries

Page 11: Naturalists at Large: Plate tectonics

Divergent BoundariesDivergent Boundaries

• Boundary between two plates that are moving apart or rifting

• RIFTING causes SEAFLOOR

SPREADING

Page 12: Naturalists at Large: Plate tectonics

Features of Divergent Features of Divergent BoundariesBoundaries

• Mid-ocean ridges

• rift valleys

• fissure volcanoes

Page 13: Naturalists at Large: Plate tectonics
Page 14: Naturalists at Large: Plate tectonics
Page 15: Naturalists at Large: Plate tectonics
Page 16: Naturalists at Large: Plate tectonics

Convergent BoundariesConvergent Boundaries

• Boundaries between two plates that are colliding

• There are 3 types…

Page 17: Naturalists at Large: Plate tectonics

Type 1Type 1• Ocean plate colliding with a

less dense continental plate• Subduction Zone: where the

less dense plate slides under the more dense plate

• VOLCANOES occur at subduction zones

Page 18: Naturalists at Large: Plate tectonics
Page 19: Naturalists at Large: Plate tectonics

Andes Mountains, Andes Mountains, South AmericaSouth America

Page 20: Naturalists at Large: Plate tectonics

Type 2Type 2

• Ocean plate colliding with another ocean plate

• The less dense plate slides under the more dense plate creating a subduction zone called a TRENCH

Page 21: Naturalists at Large: Plate tectonics
Page 22: Naturalists at Large: Plate tectonics

Aleutian Islands, AlaskaAleutian Islands, Alaska

Page 23: Naturalists at Large: Plate tectonics

Type 3Type 3

• A continental plate colliding with another continental plate

• Have Collision Zones:–a place where folded and thrust

faulted mountains form.

Page 24: Naturalists at Large: Plate tectonics
Page 25: Naturalists at Large: Plate tectonics
Page 26: Naturalists at Large: Plate tectonics

Transform Fault BoundariesTransform Fault Boundaries

• Boundary between two plates that are sliding past each other

• EARTHQUAKES along faults

Page 27: Naturalists at Large: Plate tectonics
Page 28: Naturalists at Large: Plate tectonics

San Andreas Fault, CASan Andreas Fault, CA

Page 29: Naturalists at Large: Plate tectonics

Causes of Plate Causes of Plate TectonicsTectonics

Page 30: Naturalists at Large: Plate tectonics

Convection CurrentsConvection Currents

• Hot magma in the Earth moves toward the surface, cools, then sinks again.

• Creates convection currents beneath the plates that cause the plates to move.

Page 31: Naturalists at Large: Plate tectonics