The solid inner core is located about 3,200 miles below Earth's crust. The liquid outer core separates the solid inner core from the semi-solid mantle, allowing the inner core to rotate at a different speed from Earth's rotation.
Yi Yang and Xiaodong Song studied the seismic waves from earthquakes that have passed through the Earth’s inner core along similar paths since the 1960s to infer how fast the inner core is spinning.
However, the speed of this rotation, and whether it varies, is debatable, according to Hrvoje Tkalcic, a geophysicist at Australian National University who was not involved in the study. The inner core, he said, "doesn't come to a full stop."
According to him, the study's findings "mean that the inner core is now more in sync with the rest of the planet than it was a decade ago when it was spinning a bit faster." "There is nothing cataclysmic going on," he added.