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The Internal Processes (Chapter 14) The Internal Processes Crustal Rearrangement Plate Tectonics Vulcanism Folding and Faulting Earthquakes Crustal Rearrangement Plasticity Continental Drift Isostacy 1 Continental Drift – lateral motion of the crust: Pangea Figure 14-3 Continental Drift Figure 14-4 Isostasy – vertical motions of the crust Figure 14-2 2 Plate Tectonics Seafloor Spreading Plate Boundaries Divergent Convergent Transform Continental Rearrangement Accreted Terranes and Hot Spots Divergent Plate Boundary Sea-Floor -Seafloor Spreading Spreading Figure 14-6 Divergent Plate boundaries Figure 14-6 3 Divergent Plate boundaries Convergent plate boundary -Subduction Figure 14-7 Convergent plate boundary -Subduction Figure 14-7 4 Transform Plate Boundary Figure 14-13 Contemporary Plates Formation of Hot Spot Figure 14-17 5 The Hawaiian Hot Spot Figure 14-18 Splitting a continent - rifting Figure 14-10 Joining continents Collision ! (not convergence) Orogeny Figure 14-11 6 Formation of Accreted Terrane Figure 14-16 Accreted Terranes, Rocky Mountains Figure 14-16 Breakup of Pangaea Figure 14-4 7 Volcanism Volcanism Types of Volcanoes Shield Volcano Lava Dome Composite Volcano Cinder Cone Volcanic Hazards Distribution of Active Volcanoes Figure 14-20 Shield Volcano Figure 14-24(b) 8 Lava dome Figure 14-24(c) Composite Volcano Figure 14-24(d) Cinder Cone Figure 14-25 9 Caldera Figure 14-27 Crater Lake, Oregon Volcanic Hazards Figure 14-A 10 Igneous Intrusions Volcanic neck, Ship Rock, NM Figure 14-29 Igneous Intrusions Figure 14-31 Igneous Intrusions in the western US and Canada Figure 14-30 11 Deformation in the Earth Folding and Faulting Types of Folds Monoclines, Anticlines, and Synclines Overturned and Overthrust Folds Types of Faults Normal Reverse Strike-Slip Thrust Faulted Landforms Folding Figure 14-32 Types of Folds Figure 14-33 12 Folds Faults Figure 14-40 Types of Faults Figure 14-40 13 Landforms associated with active normal faults Rift Valley Figure 14-42 Wildrose graben, southern California 14 Landforms associated with active strike slip fault Figure 14-41 Active strike slip fault Figure 14-38 Earthquakes Earthquake Movement Magnitude and Shaking Intensity Hazards Prediction 15 Earthquake generation on faults Figure 14-E Seismic waves Earthquake magnitude •Magnitude scale: amount of energy received 100 km from epicenter •Scale is logarithmic: Increase 1 unit = 10 times greater shaking Increase 1 unit = 31 times energy release 16 Distribution of Earthquakes Figure 14-E End 17