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Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure and Materials

Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

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Page 1: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

Table of Contents

Earth’s Interior

Convection and the Mantle

Classifying Rocks

Igneous and Metamorphic Rock

Sedimentary Rocks

The Rock Cycle

Earth’s Structure and Materials

Page 2: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

WavesPaths of ocean waves change when the waves reach an island.

Earth’s Interior

Page 3: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

Earth’s CrustThe circle graph shows the composition of Earth’s crust.

Earth’s Interior

Page 4: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

Mantle PieceEarth’s mantle is nearly 3,000 kilometers thick. The rigid lithosphere rests on the softer material of the asthenosphere.

Earth’s Interior

Page 5: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

Order of Earth’s Layers

• Crust

• Mantle (lithosphere which includes crust and asthenosphere)

• Outer Core

• Inner Core

Page 6: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

Temperature Inside EarthThe graph shows how temperatures change between Earth’s surface and the core. ***Can you read this graph?

Earth’s Interior

Page 7: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

Mantle ConvectionHeat from the core and the mantle itself causes convection currents in the mantle.

Convection and the MantleHow does a Lava Lamp Model Convection Currents?

Page 8: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

Rock OriginsRocks are classified by the way they formed.

Classifying Rocks

Page 9: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

How Sedimentary Rock FormsSedimentary rocks form through a series of processes over millions of years.

Sedimentary Rocks

Page 10: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

What is the proper sequence of the terms in the word bank that will show how mountains can change into sedimentary rock?

Sedimentary Rocks

Page 11: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

The Rock CycleThrough melting, weathering and erosion, and heat and pressure, the rock cycle constantly changes rocks from one type into another type.

The Rock Cycle

Page 12: Table of Contents Earth’s Interior Convection and the Mantle Classifying Rocks Igneous and Metamorphic Rock Sedimentary Rocks The Rock Cycle Earth’s Structure

The Rock Cycle

Patterns in the Rock Cycle: Surface EventsAll of the paths of the rock cycle result from only a few surface and subsurface processes. What words belong in the empty boxes in the graphic organizer?