17.3 Theory of Plate Tectonics

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Presentation transcript:

17.3 Theory of Plate Tectonics

Plate Tectonics The theory of plate tectonics states that the Earth’s crust and rigid upper mantle are broken into enormous slabs called plates These plates move in different directions and different rates

Plate Boundaries Tectonic plates interact plate boundaries At some they come together, or converge Others they move away from one another, or diverge Some move horizontally to one another

Convergent

Divergent These are place where plates are moving apart Most of these are found ion ocean floors where they form ocean ridges This is where the ocean floor spreads Scientists have measured the rate of growth of the Atlantic to be 2-3 cm/y These boundaries can also occur on land and they are called rift valleys East Africa

Transform