Compared to earthquakes at divergent boundaries, earthquakes at subduction zones are: a higher magnitude but shallower b lower magnitude but deeper c lower magnitude and shallower d higher magnitude and deeper
Compared to earthquakes at divergent boundaries, earthquakes at subduction zones are:
Compared to earthquakes at divergent boundaries, earthquakes at subduction zones are:
| a |
higher magnitude but shallower |
|
| b |
lower magnitude but deeper |
|
| c |
lower magnitude and shallower |
|
| d |
higher magnitude and deeper |
Plate tectonics is the theory that explains the movements of pieces of Earth's lithosphere called tectonic plates. The plates move over the asthenosphere of the Earth. The boundaries between the plates are classified depending upon the direction of movement of two or more plates with respect to each other. If the plates move away from each other, then the boundary formed between them is called divergent boundary. If the plates are moving towards each other, they collide and the boundary formed between them is called a convergent boundary. If the plates slide past each other, then they form transform fault boundaries.
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