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Published byArthur Riley Modified over 9 years ago
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Review of plate boundaries:
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Everything in one easy picture:
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1)DIVERGING PLATE BOUNDARY MID OCEANIC RIDGES RIFT VALLEYS VOLCANOES EARTHQUAKES Ex: mid Atlantic Ridge and African rift valley SEE PAGE 92
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Iceland:
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2) CONVERGING PLATE BOUNDARY DEEP OCEANIC TRENCHES SUBDUCTION ZONES EXTREME CONTINENTAL MOUNTAIN BUILDING Ex: Marianas Trench, Peru-Chile Trench, Himilayan mountains See page 103-104
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Oceanic VS. Continental: Peru-Chile Trench: deep water and Andes Mountains
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Andes Mountains:
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Oceanic VS. Oceanic: Marianas Trench in Pacific: very deep water
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Japan Trench fissure at 6200 m.
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Continental VS. Continental: Himilayas: extreme mountains
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Mt. Everest:
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Everest in better perspective:
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3) TRANSFORM BOUNDARIES LONG FAULT LINES EXTREME EARTHQUAKES Ex: San Andreas Fault See pg. 97
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San Andreas:
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4) SPECIAL “HOTSPOTS” Caused by hotspots in the aesthenosphere, volcanoes can appear even in the middle of a plate. As the plate moves slowly, one hotspot can create a chain of volcanoes. Best example is the Hawaiian island arc.
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Hawaiian Island Arc:
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Mauna Loa Volcano
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Mauna Loa lava flow
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WORLD TECTONIC PLATES
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WORLD TECTONIC ACTIVITY Marianas/Japan Trench Japan Hawaii Pacific N.W., Cascade Volcanoes San Andreas Fault Peru-Chile Trench Mid Atlantic Ridge, Iceland African Rift Valley Himilayan Mountains
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