1. 9.1 Continental Drift

2. I. Evidence for Continental Drift A. Pangaea i. Alfred Wegener – proposed continental drift as a theory ii. Continental Drift – continents have moved slowly to their current locations iii. Pangaea – one large landmass that broke apart 200 million years ago. iv. Pangaea means “all land” v. Continental drift was accepted long after Wegener’s death in 1930. B. Fossil Clues i. Mesosaurus found on both Africa and South America. ii. Glossopteris found on Africa, Australia, India, South America, and Antarctica.

3. C. Climate Clues i. Warm weather plants were found on Spitzbergen in the Artic Ocean. ii. Wegner hypothesized that Spitzbegen drifted from the tropic regions. iii. Glacial clues a. South America, Africa, India, and Australia were onece covered in glaciers D. Rock Clues i. Rock make up of the continents should be the same. ii. Similar rock sturctures are found on different continents. iii. Appalachian Moutnains in US are similar to Greenland and western Europe

5. II. How could continents drift? A. Although there was evidence, Wegener couldn’t explain how or why continental drift happened. B. Continental drift was rejected. C. After Wegner’s death, more clues were found. D. Seafloor spreading helped explain how continental drift could occur. Pg 251 1-3

6. 9.2 Seafloor Spreading

7. I. Clues on the Ocean Floor A. Little was known before 1950s B. Has mountains and valleys C. mid-ocean ridges form an underwater mountain range that stretches along the center

8. D. The Seafloor Moves i. Seafloor spreading a. Hot les-dense material below Earth’s curst is forced upward toward the surface b. Turns and flows sideways carrying the seafloor away c. As seafloor spreads apart, magma moves upward and flows from the cracks d. Becomes solid as it cools and forms a new seafloor e. The seafloor cools, contracts, and becomes more dense. f. Colder seafloor sinks down E. Age Evidence i. Glomar Challenger – drilling rig that allowed scientists to drill into the seafloor to obtain rock samples ii. Seafloor rocks are no older than 180 million years iii. Youngest rocks are at the mid-ocean ridges

9. F. Magnetic Clues i. Earth’s magnetic field has a north and a south pole ii. Magnetic lines leave Earth near the north pole and enter near the south pole iii. Magnetic reversal – magnetic forces run the opposite way iv. Earth’s magnetic field has reversed many times v. Iron-bearing minerals show the reversal of magnetic field vi. Magnetic reversals form parallel strips to the mid-ocean ridges

10. 9.3 Plate Tectonics

11. I. Plate Tectonics A. Plate Movements i. 1969s – combined continental drift and seafloor spreading. ii. Plate tectonics – Earth’s crust and upper mantle are in sections that move. iii. Plates – the sections of the Earth’s crust and upper mantle B. Composition of Earth’s Plates i. Lithosphere – crust and part of the upper mantle ii. Asthenosphere – plastic like layer below the lithosphere iii. Plates of the lithosphere “float” on the asthenosphere

12. II. Plate Boundaries A. Plates Moving Apart i. Divergent boundary a. Seafloor spreading ii. North American pate is moving away from the Eurasian and African plates – Mid-Atlantic Ridge iii. Great Rift Valley in eastern Africa B. Plates Moving Together i. Convergent boundary ii. 3 types a. Subduction zone – oceanic plate forced under a continental plates and volcanoes form b. Two seafloor plates collide, one sinks, new magma forms island arc of volcanoes c. Two continental plates collide, forming mountain ranges. Earthquakes are common

13. C. Plates Sliding Past Each Other i. Transform boundaries a. Two plates slide past one another, either in the same directions at different rates or opposite directions b. Pacific plate and North American plate form San Andreas Fault