Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents...

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Plate Tectonics

Transcript of Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents...

Page 1: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Plate Tectonics

Page 2: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Earth’s Layers

Page 3: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

The crust• Lithosphere- rigid, top of the mantle and

continents• Asthenosphere- softer and hotter layer

underneath• They move like pavement resting on hot tar

Convetion Currents in the Earth's Crust

Page 4: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

The lithosphere looks like a jigsaw puzzle…on the surface of the earth

• Tectonic plates- large slabs of rock parts of ocean crust and continents rest on.

Page 5: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Geologists

• Geologists study earth processes such as landslides, earthquakes, floods and volcanic eruptions.

• Geologists work to understand the history of our planet. The better they can understand Earth’s history the better they can foresee how events and processes of the past might influence the future.

Page 6: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Alfred Wegener• A geologist who first proposed

continental drift theory in 1912• His hypothesis was that all of earth’s

continents were once one giant land mass

• Gradually they drifted apart• His scientist peers and friends did

not agree until the middle of the 1900’s

Page 7: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Evidence for Continental Drift• 1. Fossil Record: the fossil of the same ancient

reptile was found in both South America and southern Africa, but no other place in the world. Both continents must have been joined together at some time in the past.

Page 8: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Evidence for Continental Drift• Evidence of Climate change- • Fossils of ancient ferns from

jungles exist on Greenland, which is now covered in ice. Greenland must have once been near the equator.

• Evidence of glaciers existed in South Africa, where the climate is now a jungle and desert in parts.

Page 9: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.
Page 10: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Evidence for Continental Drift• Geology- rock typing found on different

continents matches up. Rocks from Brazil matches up with Africa.Carbonado diamondites supernova rocks that impacted on Earth in the Brazil and Central African Republic area (these were originally next to each other, before the ancient Gondwana continent rifted apart).

Page 11: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Rock Evidence

Page 12: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

SuperContinents• Pangaea was formed 270 mya during the

Permian and Triassic time periods of Earth’s history.

• Most of the dry land was joined together into one huge land mass.

• The Permian mass extinction, which wiped out an estimated 96% species about 248 million years ago, was a major event during this time.

• Pangaea began to split apart 200 myahttp://Pangaea

Page 13: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

New Technology, New Discoveries

• Scientists began mapping the sea floor• Using drilling, SONAR, lasers bounced off of

satellites, and undersea explorers, they started making detailed maps of the sea bed.

• These discoveries gave evidence of continental drift and how the tectonic plates moved.

Page 14: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.
Page 15: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Sea Floor Spreading

• Molten rock rises through cracks• It cools and forms new crust• Old crust is pulled away• Oldest crust is pulled down into trenches into

asthenosphere and destroyed. Called Subduction

• So…Sea floor is only 180 million years old• Earth continents are 4 billion years old

Page 16: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Sea floor spreads because of…Convection Currents

Page 18: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Divergent Boundary• Where plates move apart• Can form Rift Valley on land

Page 19: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Divergent BoundaryExample: divergent plate boundary is the Red Sea.

Once, the Arabian peninsula and Africa formed a single continent.

They are now being ripped apart. The white arrows show the directions the two plates are moving. You can see that a new ocean, the Red Sea is being formed as they separate.

Page 20: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Convergent Boundary

Page 21: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Convergent Boundary

• The dense, leading edge of the oceanic plate actually pulls the rest of the plate into the flowing asthenosphere and a subduction zone is born! Where the two plates intersect, a deep trench forms.

• Volcanoes and mountain ranges usually occur along these boundaries.

• Think Ring of Fire, Swiss Alps, Appalachian Mountains!

Page 22: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Transform Boundary

• Two plates scrape past each other• Usually form along plate lines

Page 23: Plate Tectonics. Earth’s Layers The crust Lithosphere- rigid, top of the mantle and continents Asthenosphere- softer and hotter layer underneath They.

Transform Boundary

• Example of Transform Boundary would be the San Andreas Fault in California

• Earthquakes usually happen along transform boundaries.