plate tectonics

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Plate Tectonics Environmental Science

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Plate Tectonics. Environmental Science. Plate Tectonics. The Earth Inside Out Bathymetry and Seafloor Mapping The Theory of Continental Drift Lab continental drift Seafloor Spreading Lab seafloor spreading Plate Tectonics Lab plate tectonics. Earth’s Internal Layers. - PowerPoint PPT Presentation

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Page 1: Plate Tectonics

Plate TectonicsEnvironmental Science

Page 2: Plate Tectonics

Plate TectonicsThe Earth Inside Out

Bathymetry and Seafloor MappingThe Theory of Continental Drift

Lab continental drift

Seafloor SpreadingLab seafloor spreading

Plate TectonicsLab plate tectonics

Page 3: Plate Tectonics

Earth’s Internal LayersHow do we classify the Earth’s internal layers?How is the lithosphere different from the crust?

Page 4: Plate Tectonics

Layers of the Earth

Page 5: Plate Tectonics

Composition, Density and Temp.Core: Nickel (Ni), Iron (Fe) and other heavy

elementsInner core and outer core same temperature

however massive pressure and density keeps inner core solid

Mantle: mostly Silicon (Si) and Oxygen (O)Lower density than coreLower mantle is solid, upper mantle is “plasticy”

Page 6: Plate Tectonics

Lithosphere and Asthenosphere

Page 7: Plate Tectonics

Lithosphere and AsthenosphereLithosphere = Crust and upper part of upper

mantleAsthenosphere = lower part of upper mantleLithosphere “floats” on asthenosphere

Page 8: Plate Tectonics

Rock CycleWhat are the three types of rock? How does the

rock cycle account for their formation?

Page 9: Plate Tectonics
Page 10: Plate Tectonics
Page 11: Plate Tectonics

Isostatic EquilibriumHow does Archimedes Principle relate to the

structure of the Earth?What is isostatic equilibrium?What links some earthquakes with isostatic

equilibrium? Where do such earthquakes occur?

Page 12: Plate Tectonics

Archimedes Principle

Page 13: Plate Tectonics

Archimedes Principle

Page 14: Plate Tectonics

Isostatic Equilibrium

Page 15: Plate Tectonics

IsostasyThe lithosphere floats

on the asthenosphere The various portions of

the Earth’s crust reach gravitational equilibrium

Due to variations in thickness and density, some crustal blocks ride higher than others

Page 16: Plate Tectonics

Isostatic ReboundIsostatic Equilibrium is the balance between

the weight of the lithosphere and the buoyant force of the asthenosphere

Isostatic Rebound is when compensation occurs from an increase or decrease of lithospheric weight…causing earthquakes along weak areas called - faults

Page 17: Plate Tectonics
Page 18: Plate Tectonics

Onto the Festivities!!!

Page 19: Plate Tectonics

Alfred Wegner and Continental DriftWhat is Pangea and Panthalassa?What is the theory of continental drift?What evidence did Wegner use to support his

theory?Why didn’t scientists support his theory? What

further evidence could have strengthened his theory?

Page 20: Plate Tectonics

Pangea

Panthalassa

Page 21: Plate Tectonics

Wegner’s TheoryPangea: big supercontinentPanthalassa – Ocean surrounding PangeaWegner theorized that because the less dense

continents floated on the more dense matle, Pangea broke apart into separate pieces.

Theory of Continental Drift

Page 22: Plate Tectonics

The EvidencePieces fit together like a puzzle

Page 23: Plate Tectonics
Page 24: Plate Tectonics

Fossil Distribution

Page 25: Plate Tectonics

Accepted Theory? I Think Not!Good evidence but no go for public acceptance.Possibly because Alfred was a meteorologist not a

geologistTo many gaps between continentsHe disappeared on an expedition in 1930 in

GreenlandLater on, plate tectonics theory described how the

gaps between the continents were continental shelves

Page 26: Plate Tectonics

O.k. Let’s Check It Out

Pangea Lab!!!!Oooooh Yeah Baby!

Page 27: Plate Tectonics