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Evidence for Plate Tectonics Seafloor mapping using sonar initiated during World War II provided evidence of drifting continents This caused scientists.

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Presentation on theme: "Evidence for Plate Tectonics Seafloor mapping using sonar initiated during World War II provided evidence of drifting continents This caused scientists."— Presentation transcript:

1 Evidence for Plate Tectonics Seafloor mapping using sonar initiated during World War II provided evidence of drifting continents This caused scientists to reexamine continental drift

2 There are a dozen or so major plates and several smaller ones Move in different directions and at different rates

3 Sea floor Spreading Seafloor mapping revealed mid-ocean ridges and ocean trenches Harry Hess (1960) proposed the idea of seafloor spreading Ocean crust is created at mid-ocean ridge It is split and carried away then replaced by rising magma

4 Sea-floor Spreading and Plate Boundaries

5 Older ocean floor is destroyed at oceanic trench (deepest parts of the ocean) The plate bends downward and slowly plunges back into the earth in a process called subduction This takes place at the subduction zone Most earthquakes occur at edges of plates (plate boundaries)

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7 Sea-floor Spreading and Plate Boundaries

8 Plate Boundaries Where plates interact 3 types

9 Break up of Pangaea

10 Lithosphere plate boundaries Fig. 3-20

11 1. Divergent Boundaries Places where 2 plates are moving apart Most found on the seafloor, where they form ocean ridges Where new ocean crust is formed (basalt)

12 High heat flow, volcanism, and earthquakes Causes an ocean basin to grow wider Can occur on a continent, such as East Africa (Rift Valley) May eventually lead to formation of a new ocean

13 2. Convergent Boundaries Where 2 plates move toward each other 3 types, classified by type of crust: A. Oceanic-Oceanic May result in subduction Creates a volcanic island arc and deep-sea trench

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15 B. Oceanic-Continental Subduction of oceanic produces a trench and a volcanic arc (mountain range on continent) C. Continental-Continental Forms mountain ranges such as the Himalayas

16 Converging Margins: India-Asia Collision

17 Sea-floor Spreading and Plate Boundaries

18 3. Transform Boundaries Crust is not formed or destroyed, but deformed or fractured Usually offset ocean ridges Rarely on continents – San Andreas Fault is the best known exception responsible for most of the earthquakes that strike CA each year

19 Transform Faults


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