1. 8th Grade Dynamic Earth (Mod E) U4L2: Plate Tectonics

2. Evidence for Continental Drift
Puzzle-like fit of continents.
Similar fossils on widely separated continents.
ex. Mesosaurus (swimming reptile)
Glossopteris (fern tree)

3. Climate clues
Remains of warm-weather plants in Arctic areas.
Glacial deposits in tropical areas.
Rock clues
Similar rock structures on different continents

4. - Drifting Continents
Interactive evidence for plate tectonics -

5. Pangea History
245 mya (million years ago) – Pangea formed – ocean Panthalassa around it
200 mya – Pangea breaks into Laurasia (becomes N. America and Eurasia) and Gondowana (one part S. America & Africa, one part Antarctica, Australia and India)

6. Pangea History (con’t)
150 mya – Africa & South America break apart. India, Australia & Antarctica separate
India breaks away from Austrailia and moves toward Eurasia
50 mya – India collides with Eurasia, starts Himalayan Mountains

7. How could continents drift?
Pangaea animation -

8. Continental Drift Hypothesis
Continents have moved slowly to their current locations.
Proposed by Alfred Wegner in He said all continents were once connected into one large landmass called Pangaea (meaning “all land”).
Glencoe Video 297AA on Pangaea
– The posthumous triumph of Alfred Wegener

9. Wegner’s hypothesis of continental drift was rejected by most scientists of his time because he could not explain how or why continents had moved.
After his death advances in technology resulted in new ideas that supported his hypothesis.

10. Mapping the Ocean Floor
Scientists during World War II introduced the use of sound waves to detect submarines.
In 1940’s and 1950’s scientists used sound waves on ships to map large areas of the ocean floor.

11. Using sound waves scientists discovered a system of underwater mountain ranges called the Mid-ocean Ridges.
Do Video clip Seafloor spreading (P)

12. Seafloor Spreading
Suggested by Harry Hess in 1960’s to explain the ridges.
Hot, less dense material below the Earth's crust rises upward to the surface at Mid-ocean Ridges. Then it flows sideways, carrying seafloor away from the ridge in both directions.
Seafloor spreading interactive -
Really good seafloor spreading animation –
Midocean ridge photo -

13. Evidence for Seafloor Spreading:
1968 – Glomar Challenger, a research ship, drilled into the seafloor to obtain rock samples. Discovered that the youngest rock is closest to the Mid-Ocean Ridge. Note: The submersibles also found exotic life.

14. Magnetic alignment of rocks, in alternating strips that run parallel to ridges, indicates reversals in Earth’s magnetic field.
Video – Magnetic Reversals and Sea Floor Spreading -

15. - Sea-Floor Spreading

16. Theory of Plate Tectonics
Earth’s crust & part of the upper mantle are broken into sections called plates which move around on the plastic-like mantle (asthenosphere).
Plates are made of sections containing both seafloor and continents.
Tectonic Activities:
* earthquakes
* volcanoes
* mountain building
Glencoe video on plates (Chapter 10 – ES0308AA)
Rap Battle – 5th grade -

17. Types of Plate Boundaries: .
Divergent
* 2 plates move apart
* ex. 1) Mid-Atlantic Ridge
2) Great Rift Valley in Eastern Africa (formed Red Sea)
Divergent plate boundaries occur when two plates are pulled apart. In most cases a continental is rifted apart and oceanic crust is formed between the rifted continents. Crust is created at divergent boundaries.
Watch the interactive animation below.

18. 2. Convergent 2 plates collide 3 types of convergent:
1) Oceanic-continental plates
* denser oceanic plate sinks under
continental plate forming
subduction zone and volcanic arc.
(area where plate descends (line of volcanoes on continent)
into mantle & melts) Ex. Cascade Range
Andes Mt. (SA)
Convergent boundaries animation (there’s a quiz, too!)
Go to right after “Types of Plate Boundaries
There are three types of ways in which plates interact, called plate boundary types. They are described here.
Convergent plate boundaries occur when two plates are pushed together or subducted. In most cases an oceanic plate is pushed under the less dense continental crust, and in others one oceanic plate is subducted under another. Crust is destroyed at convergent boundaries.
Watch the interactive animation below.”

19. Two Converging Oceanic Plates
* One plate bends and slides under the other plate forming a subduction zone.
* Result is a deep sea trench and an
ex. Marianna Trench
island arc of volcanoes.
ex. Japanese Islands

20. - The Theory of Plate Tectonics

21. Two converging continental plates
* Since both continental plates are less dense than the asthenosphere, usually no subduction occurs. The plates collide, crumble up, and form mountains.
ex. Himalayan Mts. (India)
Same website has a continent-continent convergent animation. AND quiz. Look for
“Continental collision occurs occasionally when the subducted oceanic crust is consumed and the two continents on each converging plate collide. Many of the major mountain belts in the world were caused by this process. The Appalachians and Himalayas are two such examples.

22. * ex. San Andreas Fault (CA) p. 284
Transform
* Plates slide past each other in opposite direction or in the same direction at different rates of movement.
* ex. San Andreas Fault (CA) p. 284
Called “oblique slip” boundary in animation AND there’s a quiz

23. Cause of Plate Tectonics:
Convection current inside Earth. The cycle of heating, rising, cooling, and sinking of material inside Earth (mantle) is thought to be the force behind plate tectonics.

25. What type of tectonic activity occurs at each type of boundary?
Divergent = earthquake, volcano (Mid-ocean ridge
Transform = earthquake
Convergent
Ocean-continent = earthquake, volcano in form of volcanic arc
Ocean-Ocean = earthquake, volcano in the form of an island arc
Continent-continent = earthquake, mountain