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
Geologic Time Scale Figure 8.1
Earth’s Structure and Internal Energy Earth in Cross Section Earth’s core Earth’s magnetism Earth’s mantle Lithosphere and crust
Earth in Cross Section Figure 8.2
Earth’s Interior Figure 8.2
Earth’s Interior Figure 8.2
Earth’s Interior Figure 8.2
Core to Crust Figure 8.3
Isostatic Adjustment Figure 8.4
The Geologic Cycle The Rock Cycle Igneous processes Sedimentary processes Metamorphic processes
The Geologic Cycle Figure 8.5
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
Cubic Crystals of Pyrite Figure 1.7 A
Elemental Abundances in Continental Crust Figure 1.14
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
Table 1.1
Quartz (SiO2) Exhibits a Variety of Colors
The Rock Cycle Figure 8.6
Igneous Rock Types Figure 8.7
Intrusive and Extrusive Rocks Figure 8.8
Course-Grained Igneous Texture Figure 2.4 B
Sedimentary Rock Types Figure 8.9
Metamorphic Rocks Figure 8.12
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
Crustal Movements Figure 8.13
Continents Adrift Figure 8.15
Magnetic Reversals Figure 8.14
Ocean Floor Figure 8.17
Earth’s Major Plates Figure 8.16
Earthquakes and Volcanoes Figure 8.18
Hot Spot Tracks Figure 8.19
Elemental Geosystems 5e End of Chapter 8 Elemental Geosystems 5e Robert W. Christopherson Charles E. Thomsen