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Exploring Geography CHAPTER 1
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Section 2 Changes Within the Earth Objectives:
Describe both the internal and external structures of the Earth. Explain how forces inside the earth create and change landforms. Summarize the main ideas of plate tectonic theory.
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- the study of the earth’s physical structure and history.
Geology - the study of the earth’s physical structure and history.
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Vocabulary BEFORE AFTER Key Terms: Core Mantle Crust Continents Relief
Lava Fold Faults Plate Tectonics Continental Drift Theory Ring of Fire BEFORE AFTER
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Changes Within the Earth
The Earth’s Structure Internal Forces Geologic History
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Plumbing System of a Volcano
Fig. 5.1
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Ejecta ash volcanic bombs volcanic tuff volcanic breccias
pyroclastic flow (look out!)
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Escaping a Pyroclastic Flow at Mount Unzen, Japan, 1991
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Shield Volcano Fig. 5.10
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Cinder Cone Fig. 5.12
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Composite Volcano Fig. 5.14
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Before May, 1980 Emil Muench/Photo Researchers
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After May, 1980 David Weintraub/Photo Researchers
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fissure eruption
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1971 Fissure Eruption, Kilauea, Hawaii
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Plate Tectonics: the unifying theory
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Plate Tectonics: The Unifying Theory
Peter W. Sloss, NOAA-NESDIS-NGDC
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“Fit” of the Continents
Fig. 20.1
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Pangaea 250 Million Years Ago
Fig.21.1
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Relative Motion of the Plates
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Relative Velocity and Direction of Plate Movement
Fig Data from C. Demets, R.G> Gordon, D.F. Argus, and S. Sten, Model Nuvel-1, 1990
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Age of Seafloor Crust Fig R. Dietmar Muller, 1997
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Types of plate boundaries
• divergent: mid-ocean ridges • convergent: collision zones volcanic arcs • strike-slip: San Andreas fault
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Divergent boundaries Two types: Examples:
Continent-Continent East African Rift Ocean–Ocean Mid-Atlantic Ridge
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Continental-Continental Divergent plate boundary
East African Rift Valley
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Inception of Rifting Within a Continent
Fig. 20.4b
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Cooling and subsidence of rifted margin allows sediments to be deposited
Fig b
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Gulf of ‘Aqaba Gulf of Suez
Nile Delta Gulf of ‘Aqaba Gulf of Suez Red Sea Fig. 20.5a Earth Satellite Corp.
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Oceanic-Oceanic Divergent Plate Boundary
Mid-Atlantic Ridge
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Rifting and Seafloor Spreading Along the Mid-Atlantic Ridge
Fig. 20.4a Peter W. Sloss, NOAA-NESDIS-NGDC
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Rifting and Seafloor Spreading
Fig. 20.4a
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Convergent boundaries
Three types: Examples: ocean–ocean Japan ocean–continent Andes continent–continent Himalaya
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Oceanic-Oceanic Convergent Plate Boundary
Japan
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Ocean–Ocean Subduction Zone
Fig. 20.6b
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Parts of an Ocean–Ocean Convergent Plate Boundary
Fig
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Oceanic-Continental Convergent Plate Boundary
Andes Mountains
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Ocean-Continent Subduction Zone
Fig. 20.6a
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Parts of an Ocean–Continent Convergent Plate Boundary
Fig
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Continental-Continental Convergent Plate Boundary
India & Asia
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Continent-Continent Collision
Fig. 20.6c
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Continent– Continent Collision
Fig b
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Continent–Continent Convergent Boundary
Fig. 20.d
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Indian plate subducts beneath Eurasian plate
60 million years ago Fig.21.6a
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Indian subcontinent collides with Tibet
40–60 million years ago Fig.21.6b
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Main boundary fault develops
10–20 million years ago Fig.21.6d
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Transform Plate Boundary
San Andreas Fault
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The Gulf of California Formed by Rifting of Baja California from Mainland Mexico
Fig. 20.5b Worldsat International/Photo Researchers
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Examples of Plate Boundaries
O-C convergent O-O divergent C-C divergent O-O divergent O-O convergent O-O divergent O-C convergent Fig. 20.8a,b
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