Videos A to Z
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Plate Tectonics: Mid-ocean ridge map
- 3-5
- 6-8
- 9-12
Mid-ocean ridges form the largest mountain range in the world - over 80,000 km long. » more info
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Plate Tectonics: Mid-ocean ridges video clip
- 3-5
- 6-8
- 9-12
Mid-ocean ridges are underwater mountain ranges. » more info
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Plate Tectonics: Ocean floor moving
- 3-5
- 6-8
- 9-12
Continents ride on top of drifting pieces of the ocean floor. As the ocean floor moves, the continents move. » more info
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Plate Tectonics: Pacific plate
- 3-5
- 6-8
- 9-12
The Pacific Plate is the largest of the seven major plates. » more info
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Plate Tectonics: Plate boundary
- 3-5
- 6-8
- 9-12
A plate boundary is where plates meet. This depicts a subduction zone, in which one plate is pushed under another. Subduction zones are also referred to as destructive zones because oceanic lithosphere… » more info
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Plate Tectonics: Plate interactions
- 3-5
- 6-8
- 9-12
Plates can interact in three ways: move toward one another in a convergent boundary; move away from each other at divergent plate boundaries, or slide past each other at a transform fault. » more info
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Plate Tectonics: Rift valley
- 3-5
- 6-8
- 9-12
A rift valley is a crack along a mid-ocean ridge where a lot of volcanic activity occurs. » more info
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Plate Tectonics: Seafloor spreading
- 3-5
- 6-8
- 9-12
The theory of seafloor spreading states that the seafloor is moving, causing segments to separate at mid-ocean ridges, where lava wells up from valley rifts, forming a new ocean floor. » more info
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Plate Tectonics: Subduction
- 3-5
- 6-8
- 9-12
Subduction is the process of one plate plunging beneath another plate. Volcanoes often result. » more info
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Plate Tectonics: Transform fault
- 3-5
- 6-8
- 9-12
Rocks slide past each other at transform faults, which are characterized by shallow earthquakes, but have little volcanic activity. The San Andreas fault is an example of a transform fault. » more info
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