Faint yet distinct ground motions recorded by a large network of seismic instruments in Japan in early 2006 are the strongest, most direct evidence that Earth’s inner core is solid.
On February 22, 2006, a magnitude-7 quake rocked Mozambique. The temblor was an unusually large one for southern Africa, but it also was quick for its size: Motions at the epicenter lasted only eight seconds or so, says George Helffrich, a geophysicist at the University of Bristol in England.
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