1. Plate Tectonics - PANGAEA http://www.middleschoolscience.comhttp://www.middleschoolscience.com 2009

2. Evidence of Pangea

8. Continental Drift http://members.enchantedlearning.com/subjects/astronomy/planets/earth/Continents.shtml Alfred Wegener 1900’s Continents were once a single land mass that drifted apart. Theory is called continental drift. Fossils of the same plants and animals are found on different continents Called this supercontinent Pangaea, Greek for “all Earth” 250 Million years ago Split again – Laurasia & Gondwana 180 million years ago

9. Tectonic Plates- major and minor

10. How Plates Move- convection currents in the mantle causes hot magma to rise and sinks as it cools. This movement results in the movement of the lithosphere/crust. http://pubs.usgs.gov/gip/dynamic/unanswered.html

11. Earth’s Layers The Earth's rocky outer crust solidified billions of years ago, soon after the Earth formed. This crust is not a solid shell; it is broken up into huge, thick plates that drift atop the soft, underlying mantle.

12. The Crust Outermost layer 5 – 100 km thick Made of Oxygen, Silicon, Aluminum

13. The Mantle Layer of Earth between the crust and the core Contains most of the Earth’s mass Has more magnesium and less aluminum and silicon than the crust Is denser than the crust

14. The Core Below the mantle and to the center of the Earth Believed to be mostly Iron, smaller amounts of Nickel, almost no Oxygen, Silicon, Aluminum, or Magnesium

15. Plate Tectonics “tektonikos” means “builder” in GREEK Pieces of the lithosphere that move around Float on top of mantle’s asthenosphere similar to ice cubes in a bowl of water Each plate has a name Fit together like jigsaw puzzles

16. Sea Floor Spreading Mid Ocean Ridges – underwater mountain chains that run through the Earth’s Basins Magma rises to the surface and solidifies and new crust forms Older Crust is pushed farther away from the ridge

17. Different Types of Boundaries http://pubs.usgs.gov/gip/dynamic/understanding.html

18. Divergent Boundary – Arabian and African Plates

19. Convergent Boundary – Indian and Eurasian Plates

20. Convergent Boundary – Oceanic & Continental (denser oceanic crust will dive under the less dense continental crust, creating volcanoes or trenches http://pubs.usgs.gov/gip/dynamic/understanding.htmlhttp://pubs.usgs.gov/gip/dynamic/understanding.html & http://www.geology.comhttp://www.geology.com

21. Convergent Boundary – Oceanic & Oceanic (one will dive under the other due to density. This may result in the formation of a trench or volcanoes. http://pubs.usgs.gov/gip/dynamic/understanding.htmlhttp://pubs.usgs.gov/gip/dynamic/understanding.html & http://www.geology.comhttp://www.geology.com

22. Convergent Boundaries – Continental & continental crust create mountains http://pubs.usgs.gov/gip/dynamic/understanding.html & http://www.geology.comhttp://www.geology.com

23. Transform Boundary – when 2 plates slide past each other due to friction, usually resulting in earthquakes. www.geology.com

24. Review Name the 3 main layers of the Earth What is a tectonic plate? What was Pangea? What is Sea-Floor spreading? Name the three different types of plate boundaries and one location on Earth for each one