An earthquake’s hypocenter is the position where the strain energy stored in the rock is first released, marking the point where the fault begins to rupture. This occurs at the focal depth below the epicentre.
4ESO, clil, geology
This entry was posted on October 22, 2010, 11:18 am and is filed under Geology, Internal geology. You can follow any responses to this entry through RSS 2.0.
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