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Theory Plate Boundaries Convergent Divergent Transform Hot Spots. Theory of Plate Tectonics. What is a SCIENTIFIC THEORY?. A well tested concept that explains a wide range of observations. In 1965, J. Tuzo Wilson, a Canadian scientist proposed the theory of Plate Tectonics - PowerPoint PPT Presentation
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What is a SCIENTIFIC THEORY?
A well tested concept that explains a wide range of observations
• In 1965, J. Tuzo Wilson, a Canadian scientist proposed the theory of Plate Tectonics– Combined knowledge of sea-floor spreading
with continental drift
Theory of Plate Tectonics
Earth’s lithosphere is broken into sections called plates.
Plates are always shifting and moving.
Movement is driven by convection currents in the mantle.
Evidence: All the evidence collected over the 1900’s was used in this theory.
Late 1900’s
Plate Boundary MotionCONVERGE - Moving toward one another.
connecting
DIVERGE – Moving apart.
dividing
TRANSFORM – Sliding past one another.
Plate Tectonics II Plates, Plate Boundaries, and Driving Forceshttp://www.visionlearning.com/library/module_viewer2.php?mid=66&l=&let1=Ear
Plate Boundarieshttp://www.wwnorton.com/college/geo/egeo/flash/2_6.swf
Narrative and animation by:Monte Hieb and Nancy Hieb
Convergent BoundaryOceanic Crust – Continental Crust
Features
•Subduction Zone
•Trench
•Volcanic Mountain Arc
Tectonic plates connecting
http://www.pbs.org/wgbh/aso/tryit/tectonics/convergent.html
Convergent Boundary
Continental Crust – Continental Crust
Features
•Folded Mountains
Tectonic plates connecting
http://www.pbs.org/wgbh/aso/tryit/tectonics/convergent.html
Convergent Boundary
Oceanic Crust – Oceanic Crust
Tectonic plates connecting
Features
•Subduction Zone
•Trench
•Island Arc
Narrative and animation by:Monte Hieb and Nancy Hieb
http://www.pbs.org/wgbh/aso/tryit/tectonics/divergent.html
Divergent Boundary
Features
•Mid-Ocean Ridge
•Rift Zone
Tectonic plate dividing
http://www.pbs.org/wgbh/aso/tryit/tectonics/transform.htmlhttp://www.wwnorton.com/college/geo/animations/transform_faulting.htm
Transform Boundary
Plates move in opposite directions on either side of the transform boundary, causing earthquakes.
Plates move in similar directions on either side of the fracture zone (red dashed line), resulting in fewer earthquakes.
Hot Spots
http://www.classzone.com/books/earth_science/terc/content/investigations/es0810/es0810page03.cfm?chapter_no=investigation
Magma has broken through crust as the plate moves over a spot
http://www.wwnorton.com/college/geo/animations/hot_spot_volcanoes.htm