The science of earthquakes explained
8 years, 1 month ago

The science of earthquakes explained

ABC  

Earthquakes can cause immense damage to buildings and infrastructure, trigger tsunamis, and reshape the Earth's surface with their force. The largest earthquakes happen where one plate collides and slips under another or collides with and slips past another Megathrust earthquakes Plate boundaries converge, a process that can generate earthquakes. " "Once the strain reaches a certain point, that locked section of the subduction interface will break and that's effectively what the earthquake is," Dr Allen said. Slip-strike earthquakes A separate type of earthquake is caused by a transform fault, also known as a strike-slip fault, which involves two plates sliding past each other, rather than pulling away or pushing together. "In the 2010/2011 Christchurch earthquake sequence, we saw there was a very large earthquake that occurred in September 2010, and was preceded by a very active aftershock sequence, and we continued to see large earthquakes gradually migrating along a network of faults from the west to the east," Dr Allen said.

History of this topic

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