Plate Tectonics

Transcript

1. Plate Tectonics
2. • If you look at a map of the world, you may notice that some of the continents could fit together like pieces of a puzzle.
3. CONTINENTAL DRIFT According to the hypothesis of continental drift, continents have moved slowly to their current locations.
4. Pangaea about 200 million years ago, before it began breaking up. Wegener named the southern portion of Pangaea Gondwana, and the northern portion Laurasia.
5. The continents about 70 million years ago. Notice that the breakup of Pangea formed the Atlantic Ocean. India’s eventual collision with Eurasia would form the Himalayan Mountains.
6. The position of the continents today. The continents are still slowly moving, at about the speed your fingernails grow. Satellite measurements have confirmed that every year the Atlantic Ocean gets a few inches wider!
7. Quick Check Turn and tell your neighbor who came up with the continental drift theory, and how we know it is still happening today.
8. Continents fit together like a puzzle….e.g. the Atlantic coastlines of Africa and South America. The Best fit includes the continental shelves (the continental edges under water.) Wegener’s Evidence for Continental Drift Picture from http://www.sci.csuhayward.edu/~lstrayer/geol2101/2101_Ch19_03.pdf
9. Wegener’s Evidence for Continental Drift Fossils of plants and animals of the same species found on different continents. Picture from http://volcano.und.edu/v wdocs/vwlessons/plate _tectonics/part3.html
10. Wegener’s Evidence for Continental Drift • Rock sequences (meaning he looked at the order of rock layers) in South America, Africa, India, Antarctica, and Australia show remarkable similarities. • Wegener showed that the same three layers occur at each of these places. • Picture from http://volcano.und.edu/vwdocs/vwlessons/plate_tectonics/part4. html
11. Closing: In your own words, explain what the theory of continental drift says, and provide at least one evidence for it
12. Plate Tectonics • 12 major plates move in various directions • Plates collide, pull apart, or scrape against each other. • Each type of interaction causes a characteristic set of Earth structures or “tectonic” features. • Tectonic-deformation of the crust as a consequence of plate interaction.
13. World Plates
14. What are tectonic plates made of? • Plates are made of rigid lithosphere. The lithosphere is made up of the crust and the upper part of the mantle.
15. What lies beneath the tectonic plates? • Below the lithosphere (which makes up the tectonic plates) is the asthenosphere.
16. Think-Pair-Share Make a prediction as to why you think the plates move.
17. Plate Movement • “Plates” of lithosphere are moved around by the underlying hot mantle convection cells
18. What happens at tectonic plate boundaries?
19. • Divergent • Convergent • Transform Three types of plate boundary
20. • Spreading ridges – As plates move apart new material is erupted to fill the gap Divergent Boundaries
21. Age of Oceanic Crust Courtesy of www.ngdc.noaa.gov
22. • Iceland has a divergent plate boundary running through its middle Iceland: An example of continental rifting
23. • There are three styles of convergent plate boundaries – Continent-continent collision – Continent-oceanic crust collision – Ocean-ocean collision Convergent Boundaries
24. • Forms mountains, e.g. European Alps, Himalayas Continent-Continent Collision
25. Himalayas
26. • Called SUBDUCTION Continent-Oceanic Crust Collision
27. • Oceanic lithosphere subducts underneath the continental lithosphere • Oceanic lithosphere heats and dehydrates as it subsides • The melt rises forming volcanism • E.g. The Andes Subduction
28. • When two oceanic plates collide, one runs over the other which causes it to sink into the mantle forming a subduction zone. • The subducting plate is bent downward to form a very deep depression in the ocean floor called a trench. • The worlds deepest parts of the ocean are found along trenches. – E.g. The Mariana Trench is 11 km deep! Ocean-Ocean Plate Collision
30. • Where plates slide past each other • Also called strike-slip Transform Boundaries Above: View of the San Andreas transform fault
32. Plate Tectonics Summary • The Earth is made up of 3 main layers (core, mantle, crust) • On the surface of the Earth are tectonic plates that slowly move around the globe • Plates are made of crust and upper mantle (lithosphere) • There are 2 types of plate • There are 3 types of plate boundaries • Volcanoes and Earthquakes are closely linked to the margins of the tectonic plates