The Earth's internal layers including the mantle, outer core, and inner core. USC Graphic/Edward SoteloShareEarths core is pretty dynamic. Its spin speeds up and slows down based on how its two primary layers are behaving. As we improve the waveform techniques used to study the deepest layer thousands of feet below the surface, our understanding of it continues to evolve. Now, scientists believe that Earths inner core might be less solid than we previously thought. The findings are detailed in a study published February 10 in the journal Nature Geoscience and shed light on how topographical changes might be affecting the cores rotation. Get the Popular Science newsletter Breakthroughs, discoveries, and DIY tips sent every weekday. By signing up you agree to our Terms of Service and Privacy Policy.Round and round it goesEarths core is located below the middle layer called the mantle and the outer layeror crust. It consists of two main partsa liquid outer core and a more solid inner core. The outer layer is made of liquid iron-nickel and is responsible for producing Earths magnetic field. The magnetic field and the liquid outer core are further stabilized by the more solid inner section. The inner core is made of solid iron-nickel about 3,000 miles below the surface of the Earth.Scientists believe that the inner cores rotation began to slow down in 2010, but what that really means has been up for debate. We cant really feel those changes on Earth, but when the core spins more slowly, the mantle will speed up. This shift ultimately makes the Earth rotate faster, but translates to only thousandths of a second in day length.The goal of this new study was initially to further document this slowing. However, one particular dataset on seismic waves revealed to study co-author and University of Southern California seismologist John Vidale that the inner core is not quite as solid as we thought.What we ended up discovering is evidence that the near surface of Earths inner core undergoes structural change, Vidale said in a statement.The new study used seismic waveform data, including 121 repeating earthquakes recorded from 42 locations near Antarcticas South Sandwich Islands between 1991 and 2024. This kind of data can give scientists a glimpse of what takes place in the inner core since they cant journey to the center of the Earth. The researchers analyzed the waveforms from receiver-array stations located near Fairbanks, Alaska, and Yellowknife in Canadas Northwest Territories. One dataset of seismic waves from the Yellowknife station included some uncharacteristic properties the team had never observed before.Once his research team improved their resolution technique so that they could see the data better, it was clear that these waveforms represented additional physical activity of the inner core.Disturbing the inner coreAccording to the study, this physical activity appears to be temporal changes in the shape of the inner core. The near surface of the inner core may undergo viscous deformation, or changing its shape and shifting at the inner cores shallow boundary. This interaction between the inner and outer core is likely the cause of this structural change.The molten outer core is widely known to be turbulent, but its turbulence had not been observed to disrupt its neighbor the inner core on a human timescale, Vidale said. What were observing in this study for the first time is likely the outer core disturbing the inner core.This new discovery could lead scientists to some previously hidden dynamics happening deep within Earths core. Both rotational and non-rotational changes are happening in the inner core, fundamentally changing what we once understood about this deep layer. The team believes that more investigation into these forces is needed to see what is stirring at the core and could help us better understand Earths thermal and magnetic field.