1. I-6 Dynamic Planet Notes
Activity Notes and Digging Deeper Notes

2. Evidence of a Super Continent
Continents fit together. See the match between the east coast of South America and the west coast of Africa.
Several of the world’s mountain ranges that appear on a continent today are similar in age and form to mountain ranges that are on another continent.

3. Several fossils are found on particular landmasses but not on others
Cynognathus was a reptile that lived in what are now Brazil and Africa
Lystrosaurus was found in central Africa, India, and Antarctica
Glossopteris was a fern found in Antarctica, Australia, India, Southern Africa, and South America

4. Mesosaurus was found in the southern tip of South America and the southern tip of Africa

5. Evidence produced by glaciers from long ago provide geoscientists with ideas about the movement of continents.
Like a bulldozer, a glacier plows a large pile of rock and sediment. When the glacier melts, the “plowed” deposit, called a terminal moraine, is left at the front of the glacier

6. Evidence of ice sheets 300 million years old has been found in the southern hemisphere

7. Super Continent

8. Digging Deeper Notes

10. Continental Drift
Believed over 100 years ago based on observation of how Africa and South America fit together-Perhaps was once a single continent
Idea is that the single continent broke apart and the pieces drifted away from each other to form the Atlantic Ocean

11. Theory not accepted by geoscientists until the 1960’s
The Theory of Plate Tectonics gave a natural explanation for continental drift

12. Supercontinents
Geoscientists are sure that about 250 million years ago all of the Earth’s continents were gathered into a single “supercontinent”
Formed by a series of continent-continent collisions
Named Pangea (“Pan” means “all”, and “gea” means “land”)

13. Suture Zones Evidence for the existence of Pangea
Former continent-continent collisions
Are found in the interiors of continents
Believed to be where earlier continents joined to form Pangea
Example, the Appalachian Mountains in North America

14. The Breakup of Pangea
About 200 million years ago the pattern of convection cells in the mantle changed
Caused Pangea to slowly split apart
Process is called continental rifting
Caused the Atlantic, Indian, and Antarctic Oceans to grow larger
Rifts didn’t develop in the same places where Pangea was first sutured together

15. There is evidence of earlier supercontinents
There is evidence of earlier supercontinents. One may have existed about 600 million years ago.
At the time of Pangea, the Pacific Ocean was the only ocean! (Pacific Ocean is surrounded by subduction zones and is being consumed

16. Prediction for the Future
Pacific ocean will continue to shrink until all of today’s continents collect to form a new supercontinent OR
The pacific ocean will expand again, and the new oceans will close up again to form a Supercontinent where Pangea once existed (Scientists believe the latter)

17. The measurement of plate movement is made by using a satellite-based global positioning system (GPS)

18. I-6 AYR Questions
In your own words, explain the theory of continental drift.
What was Pangea?
How is a suture zone formed?
Why is the Pacific Ocean shrinking?

19. Answers to AYR
1. According to plate tectonic theory, the outermost layer of the Earth consists of pieces of lithosphere called plates. The plates move relative to one another. Some of the plates have continents on them. The continents move relative to one another.

20. 2. Pangea (Pangaea) was a continent that existed about 250 million years ago. It consisted of all of the Earth’s continents, which had been gathered by continental drift into a single large continent, called a supercontinent.

21. 3. A suture zone is the place where two separate continents come together to form a single continent. Suture zones form at continent-continent collision zones.

22. 4. The Pacific Ocean is shrinking because there are subduction zones all around it. Oceanic lithosphere is being consumed at those subduction zones. There are mid-ocean ridges in the Pacific also, but the rate of production of new oceanic lithosphere there is less than the rate of consumption of oceanic lithosphere at the subduction zones, so Pacific is shrinking.