chapter 7 section 1: continental drift section 2 : sea floor spreading section 3: plate tectonics
TRANSCRIPT
Chapter 7 Chapter 7
Section 1: Continental DriftSection 1: Continental Drift
Section 2 : Sea Floor SpreadingSection 2 : Sea Floor Spreading
Section 3: Plate TectonicsSection 3: Plate Tectonics
Section 1 Continental DriftSection 1 Continental Drift
• Alfred Wegener– (1880-1930)– Proposed hypothesis of continental drift– Pangaea
Evidence to support C.D.Evidence to support C.D.
• Continents appear to fit together like a puzzle
• Similar fossils have been found on different continents
• Remains of warm climate plants in arctic zones and Arctic clues in tropical zones
• Similar rock structures found on different continents
Section 2: Seafloor SpreadingSection 2: Seafloor Spreading
• Magma below Oceanic crust pushes upward and outward forcing the crust into large underwater mountain ranges.
• Mid Ocean Ridges
Evidence for S.F.SEvidence for S.F.S
• A theory– Has been proven to occur
• Rocks increase in age as one moves away from the mid-ocean ridges.
• Continents are measure farther apart by 1 or 2 inches per year
old new
Section 3: Theory of Plate Section 3: Theory of Plate TectonicsTectonics
• Combines the hypothesis of continental drift with the theory of sea floor spreading.
• Earth’s crust and upper mantle broken into plates.
• Shift on layer of molten rock.
Earth’s platesEarth’s plates
• Lithosphere– Earth’s crust and upper mantle– Layer that shifts
• Asthenosphere– -like layer
of mantle.
Earth’s crustEarth’s crust
• Continental crust– Thick– Less dense– Older– Forms land
• Oceanic crust– Thin– Dense– Younger– Forms ocean bottom
Plate BoundariesPlate Boundaries
• Divergent– Where 2 plates move apart– Sea floor spreading!– Mid-Atlantic ridge– Rift Valley
Plate Boundaries contd.Plate Boundaries contd.• Convergent Boundary
– Where 2 plates move together.– Oceanic / Continental plate collision– Subduction
zone.– Volcanic
Mtns.– Trench
Convergent Boundaries contd.Convergent Boundaries contd.
• Continental / Continental crust collision– Forms mountains– India plate moving north / Eurasian plate
moving south.• Himalayan Mountains
• Oceanic/Oceanic convergent collision.
• Creates a trench
• Both subducted, but one more than the other
Transform BoundariesTransform Boundaries
• 2 plates sliding past each other
• Strike-slip faults
• Can move in different directions or the same direction at different rates.
• San Andreas Fault in California.– Earthquake zone
Causes of Plate movement.Causes of Plate movement.
• Convection Currents– The heating, rising, cooling, and falling cycle
of molten rock in the earth’s mantle.