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STUDY QUESTIONS |
Interactions between the asthenosphere and the lithosphere create most of the major features at the surface of the earth. Upwelling and convection cells in asthenosphere cause the lithosphere to break into pieces called plates, that move, and, in turn, interact mostly at their boundaries. This creates distinctive sets of features with each boundary type.
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A. DIVERGENT either on cont or ocean
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Ridge systems
Rift Vulcanism- ranges from isolated volcanos to basalt plateaus Shallow focus Earthquakes*** |
E. Africa Rift Valley
Red Sea Mid Ocean Ridges in all oceans |
B. CONVERGENT
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Oceanic lithoshere subducted
Subduction Zone Accretionary wedge (=prism) Vulcanism on up plate-Vulcanic Island arc w/ associated trench Trench Shallow, Intermediate and Deep focus Earthquakes |
Aleutians Islands
Phillipines Islands Mariannas Islands Windward Islands of Carribean |
2. Ocean/Continent Convergence | Oceanic litho subducted
Subduction Zone Accretionary wedge (=prism) Vulcanism on up (=cont.) plate Marginal Mountains on up plate (=cont) Trench Shallow, Intermediate and Deep focus Earthquakes |
Andes
Alaska Peninsula SE Asia: Java, Sumatra , etc |
3. Continent/Continent Convergence | Neither plate subducted
Internal Mountains Underplating Shallow and Intermediate focus Earthquakes (No vulcanism) |
Himalayas
Urals Appalachians |
C. TRANSFORM
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Transform Faults
Shallow focus Earthquakes |
California
Central America |
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Hot Spots. Primary indicator is vulcanism.
Vulcanic Island arcs w/o associated trenches or basaltic plateaus. |
Yellowstone
Iceland Hawaiian Islands and Emperor Sea Mounts |
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Transform Faults | Asian Continent
Across ridges in oceanic plates |