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Chapter 4 Lesson 1 Plate Tectonics

Chapter 4 Lesson 1 Plate Tectonics

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Chapter 4 Lesson 1 Plate Tectonics. What Are Earth’s Layers. Core - central part Inner Core – solid metals Outer Core – liquid metals. Mantle – thick layer of solid and molten rock that surrounds the core Lower – solid rock Upper – 2 parts Lithosphere – solid- upper mantle & crust - PowerPoint PPT Presentation

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Page 1: Chapter 4 Lesson 1 Plate Tectonics

Chapter 4Lesson 1

Plate Tectonics

Page 2: Chapter 4 Lesson 1 Plate Tectonics

What Are Earth’s Layers

Page 3: Chapter 4 Lesson 1 Plate Tectonics

Earth’s Layers

• Core- central part– Inner Core – solid

metals– Outer Core – liquid

metals

• Mantle – thick layer of solid and molten rock that surrounds the core

• Lower – solid rock• Upper – 2 parts

• Lithosphere – solid- upper mantle & crust

• Asthenosphere – upper mantle – melted rock

Page 4: Chapter 4 Lesson 1 Plate Tectonics

• Crust– Thin layer of solid rock

that makes up the outermost layer.

– Where we live

• Atmosphere – – All gases that

surround the Earth

• Hydrosphere– All of Earth’s liquid and

solid water (lakes, oceans, rivers, glaciers)

– Covers 70% of the Earth

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Earth ~200 million years ago

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The Continental Drift Hypothesis

Geologist – person that studies rocks

Thought of by Alfred Wegener in 1915.

Continents "drifted" to their present positions.

Supercontinent Pangaea started to break up about 200 million years ago.

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Continental Drift: Evidence

Geographic fit of South America and Africa

Fossils match across oceans

Rock types and structures match across oceans

Ancient glacial features

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Tight fit ofthe

continents, especially

usingcontinental

shelves.

Continental

Drift:Evidence

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Continental Drift: Evidence

Fossil critters and plants

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Continental Drift:

Evidence

Correlation of

mountains with nearly

identical rocks and structures

Page 13: Chapter 4 Lesson 1 Plate Tectonics

ContinentalDrift:

Evidence

Glacial features

of the same age

restore to atight polar

distribution.

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Presumably,Pangaea was ripped apart

by such continental

rifting & drifting.

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What causes the continents

to move?Plate Tectonics

•Theory to explain how forces deep within Earth can cause seafloors to spread and continents to move.

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Tectonic PlatesTectonic Plates

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Continental Divergent BoundaryExample: Red Sea / E. African Rift

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•Magma – hot melted rock

• Tension – push or a stretch on the plates

•Seafloor Spreading – caused by magma pushing on the plates

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Mid Ocean RidgesMid Ocean Ridges

- underwater mountain ranges

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Subduction – when one tectonic plate can sink under

another plate- crust gets recycled back into the mantle

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Mountain Formation• Compression – a squeezing

or pushing together of the crust

This creates folded mountains.

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Fault – deep cracks in the Earth’s crust where rocks move in the opposite direction

• Fault Block Mountain – Caused by tension

when one block of rock moves down

– Sierra Nevada Mountains