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Not only is there an outer core of liquid iron encircling a Moon-size inner core of solidified iron, Dr. Ishii said, but seismic data indicate that nested within the inner core is another distinct layer they call the innermost core: a structure some 375 miles in diameter that may well be almost pure iron, with other elements squeezed out.
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Gravity modelling and seismic data indicate that the seismic velocities and the densities of the upper crust correspond to an acidic (granitic to granodioritic) composition whereas the lower crust is of mafic composition (gabbro).
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Dr. Lay said the seismic data indicates the larger earthquake occurred first, and the hidden earthquake followed less than 45 seconds later.
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