
The study, published Feb. 10 in the journal Nature, looked at earthquake waves that have skimmed the edge of the inner core, 3,200 miles (5,150 kilometers) deep. It revealed that, even when the core had rotated into a previously observed position, there were often subtle differences.
These differences suggest that the inner core's surface, while solid, could be quite changeable over short periods.
"The most likely thing is the flow in the outer core is stirring up the outermost inner core a little bit and changing the topography," said John Vidale, the leader of the study and a seismologist at the University of Southern California Dornsife.
The outer core is molten metal — mostly iron and nickel. It cushions the solid inner core, which is also mostly iron and nickel. Each year, a tiny bit of the liquid outer core crystallizes and adds to the solid inner core, which is growing at a rate of about a millimeter per year.












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