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The Theory of Plate Tectonics

The Theory of Plate Tectonics. Section 3. Bellringer. If the sea floor is spreading an average of 4 cm a year, how many years did it take New York and the northwest coast of Africa to reach their current locations, 676,000,000 cm apart?. Bellringer.

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The Theory of Plate Tectonics

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  1. The Theory of Plate Tectonics Section 3

  2. Bellringer • If the sea floor is spreading an average of 4 cm a year, how many years did it take New York and the northwest coast of Africa to reach their current locations, 676,000,000 cm apart?

  3. Bellringer • If the sea floor is spreading an average of 4 cm a year, how many years did it take New York and the northwest coast of Africa to reach their current locations, 676,000,000 cm apart? • 6,670 km= 676,000,000 cm / 4 cm/year = 169,000,000 years

  4. The Theory of Plate Tectonics • Describe the three types of tectonic plate boundaries. • Explain how scientists measure the rate at which tectonic plates move.

  5. The Theory of Plate Tectonics • As scientists’ understanding of mid-ocean ridges and magnetic reversals grew, a theory was formed to explain how tectonic plates move. • Plate tectonics is the theory that explains how large pieces of the Earth’s outermost layer, called tectonic plates, move and change shape.

  6. The Theory of Plate Tectonics • A boundary is a place where tectonic plates touch. All tectonic plates share boundaries with other tectonic plates. • The type of boundary depends on how the tectonic plates move relative to one another.

  7. The Theory of Plate Tectonics • There are three types of tectonic plate boundaries: • Convergent Boundaries • Divergent Boundaries • Transform Boundaries

  8. The Theory of Plate Tectonics • When two tectonic plates collide, the boundary between them is a convergent boundary. • What happens at convergent boundaries depends on the kind of crust at the leading edge of each tectonic plate.

  9. The Theory of Plate Tectonics

  10. The Theory of Plate Tectonics • When two tectonic plates separate, the boundary between them is called a divergent boundary. • New sea floor forms at divergent boundaries.

  11. The Theory of Plate Tectonics • When two tectonic plates slide past each other horizontally, the boundary between is called a transform boundary. • The San Andreas Fault in California is an example of a transform boundary.

  12. The Theory of Plate Tectonics

  13. The Theory of Plate Tectonics • Tectonic plate movements are so slow and gradual that you can’t see or feel them. The movement is measured in centimeters per year. • Scientists use a system of satellites called the global positioning system (GPS) to measure the rate of tectonic plate movement.

  14. The Theory of Plate Tectonics • Describe the three types of tectonic plate boundaries. • Explain how scientists measure the rate at which tectonic plates move.

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