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Evidence for Plate Evidence for Plate Tectonics Tectonics The Old Stuff and The Old Stuff and The New Stuff The New Stuff
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Page 1: Plate Tec Evidence

Evidence for Plate Evidence for Plate TectonicsTectonics

The Old Stuff andThe Old Stuff and

The New StuffThe New Stuff

Page 2: Plate Tec Evidence

Wegener’s EvidenceWegener’s Evidence

The Old StuffThe Old Stuff

Page 3: Plate Tec Evidence

Puzzle Fit ContinentsPuzzle Fit Continents

Page 4: Plate Tec Evidence

Mesosaurus FossilsMesosaurus Fossils

Page 5: Plate Tec Evidence

Mountain Range EvidenceMountain Range Evidence

Page 6: Plate Tec Evidence
Page 7: Plate Tec Evidence

Problem with Wegener’s StuffProblem with Wegener’s Stuff

Page 8: Plate Tec Evidence

New Evidence for New Evidence for Plate TectonicsPlate Tectonics

The New StuffThe New Stuff

Page 9: Plate Tec Evidence
Page 10: Plate Tec Evidence

Earthquake DataEarthquake Data

Page 11: Plate Tec Evidence

Hot SpotsHot Spots

Page 12: Plate Tec Evidence

Ocean DrillingOcean Drilling

Location Age of Rocks

Ridge Crests Youngest

Continental Margins 180 mya

Continental Crust 4.0 bya

Page 13: Plate Tec Evidence

Mantle ConvectionMantle ConvectionConvergent Divergent

Downward

Upward Arm

Slab Pull

Ridge Push

Page 14: Plate Tec Evidence

Seafloor SpreadingSeafloor Spreading

The seafloor contracts and sinks.

Crust spreads along an ocean ridge and magma fills the gap that is created.

Hot magma, which is less dense than the surrounding material, is forced toward the crust.

New seafloor moves away from the ridge, cools and becomes more dense than the material beneath it.

New seafloor forms as the magma hardens.

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Page 15: Plate Tec Evidence

Do you believe in Plate Do you believe in Plate Tectonics?Tectonics?

Page 16: Plate Tec Evidence