

Plate tectonics: The main features are:
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It is hard to imagine that these great big solid slabs of rock could wander around the globe. Scientists needed a clue as to how the continents drifted. The discovery of the chain of mountains that lie under the oceans was the clue that they were waiting for.
| PLATES ARE CREATED: In the diagram below you can see that the continental crust is beginning to separate creating a diverging plate boundary. When a divergence occurs within a continent it is called rifting. A plume of hot magma rises from deep within the mantle pushing up the crust and causing pressure forcing the continent to break and separate. Lava flows and earthquakes would be seen. In the diagram below you can see that the continental crust is beginning to separate creating a diverging plate boundary. When a divergence occurs within a continent it is called rifting. A plume of hot magma rises from deep within the mantle pushing up the crust and causing pressure forcing the continent to break and separate. Lava flows and earthquakes would be seen. |
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This is an example of a divergent plate
boundary (where the plates move away from each other). The Atlantic Ocean
was created by this process. The mid-Atlantic Ridge is an area where new sea
floor is being created.
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As the rift valley expands two continental
plates have been constructed from the original one. The molten rock
continues to push the crust apart creating new crust as it does.
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As the rift valley expands, water collects
forming a sea. The Mid-Atlantic Ridge is now 2,000 metres above the adjacent
sea floor, which is at a depth of about 6,000 metres below sea level.
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The sea floor
continues to spread and the plates get bigger and bigger. This process can
be seen all over the world and produces about 17 square kilometres of new
plate every year.
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