Chapter 8 The Dynamic Planet

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Chapter 8 The Dynamic Planet Elemental Geosystems 5e Robert W. Christophers Charles E. Thomsen

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Chapter 8 The Dynamic Planet. Elemental Geosystems 5e. Robert W. Christopherson Charles E. Thomsen. The Dynamic Planet. The Pace of Change   Earth’s Structure and Internal Energy   The Geologic Cycle   Plate Tectonics  . The Pace of Change  . Geologic Time Scale Uniformitarianism. - PowerPoint PPT Presentation

Transcript of Chapter 8 The Dynamic Planet

Page 1: Chapter 8 The Dynamic Planet

Chapter 8 The Dynamic Planet

Elemental Geosystems 5e

Robert W. ChristophersonCharles E. Thomsen

Page 2: Chapter 8 The Dynamic Planet
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The Dynamic Planet

The Pace of Change  

Earth’s Structure and Internal Energy  

The Geologic Cycle    

Plate Tectonics  

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The Pace of Change  Geologic Time Scale

Uniformitarianism

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Geologic Time Scale

Figure 8.1

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Earth’s Structure and Internal Energy  

Earth in Cross SectionEarth’s core  

Earth’s magnetism

Earth’s mantle  

Lithosphere and crust  

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Earth in Cross Section

Figure 8.2

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Earth’s Interior

Figure 8.2

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Earth’s Interior

Figure 8.2

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Figure 8.2

Earth’s Interior

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Core to Crust

Figure 8.3

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Isostatic Adjustment

Figure 8.4

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The Geologic CycleThe Rock Cycle  

Igneous processes  

Sedimentary processes  

Metamorphic processes  

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The Geologic Cycle

Figure 8.5

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Minerals: Building Blocks of Rocks

By definition a mineral is/hasNaturally occurring

Inorganic solid

Ordered internal molecular structure

Definite chemical composition

RockA solid aggregate of minerals

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Cubic Crystals of Pyrite

Figure 1.7 A

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Elemental Abundances in Continental Crust

Figure 1.14

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Mineral Groups

SilicatesMost important mineral group

Comprise most rock-forming mineralsVery abundant due to large % of silicon and

oxygen in Earth’s crust

Silicon-oxygen tetrahedronFundamental building blockFour oxygen ions surrounding a much

smaller silicon ion

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Table 1.1

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Quartz (SiO2) Exhibits a Variety of Colors

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The Rock Cycle

Figure 8.6

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Igneous Rock Types

Figure 8.7

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Intrusive and Extrusive Rocks

Figure 8.8

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Course-Grained Igneous Texture

Figure 2.4 B

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Sedimentary Rock Types

Figure 8.9

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Metamorphic Rocks

Figure 8.12

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Plate Tectonics  A Brief History  Sea-Floor Spreading and Production of New Crust  Subduction of the Crust  The Formation and Breakup of Pangaea  Plate Boundaries  Earthquake and Volcanic Activity  Hot Spots

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Crustal Movements

Figure 8.13

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Continents Adrift

Figure 8.15

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Magnetic Reversals

Figure 8.14

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Ocean Floor

Figure 8.17

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Earth’s Major Plates

Figure 8.16

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Earthquakes and Volcanoes

Figure 8.18

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Hot Spot Tracks

Figure 8.19

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End of Chapter 8

Elemental Geosystems 5e

Robert W. ChristophersonCharles E. Thomsen