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Chapter 8 The Dynamic Planet
Elemental Geosystems 5e Robert W. Christopherson Charles E. Thomsen
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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 Section Earth’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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Earth’s Interior Figure 8.2
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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 Cycle The 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/has Naturally occurring Inorganic solid Ordered internal molecular structure Definite chemical composition Rock A 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 Silicates Most important mineral group
Comprise most rock-forming minerals Very abundant due to large % of silicon and oxygen in Earth’s crust Silicon-oxygen tetrahedron Fundamental building block Four 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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Elemental Geosystems 5e
End of Chapter 8 Elemental Geosystems 5e Robert W. Christopherson Charles E. Thomsen
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