Hidden beneath layers of rock and molten metal, Earth’s inner core has long been viewed as a solid sphere. However, a recent study suggests that the surface of the inner core is undergoing structural alterations and is currently changing shape. This discovery implies that Earth’s center is far more dynamic than previously believed, potentially transforming our understanding of the planet’s evolution, its magnetic field, and its rotation.
These revelations not only deepen our knowledge of Earth’s interior but also raise intriguing questions about the forces at play beneath our feet.
Earth’s interior is like a giant layer cake with four main layers: the crust, mantle, outer core, and inner core. The crust is the thin, outermost layer where we live, and it’s broken into massive plates that constantly shift. Beneath it, the mantle extends about 1,800 miles deep and is made of hot, semi-solid rock that slowly moves. This movement drives plate tectonics, causing earthquakes, volcanic eruptions, and even the formation of mountains over millions of years.
The deeper you go, the hotter it gets, with temperatures in the mantle reaching thousands of degrees. Beneath the mantle, the outer core consists of molten iron and nickel, swirling around and creating Earth’s magnetic field. This invisible shield protects us from harmful solar radiation and keeps compasses pointing north. At the very center, the inner core is a solid ball of iron and nickel, hotter than the surface of the sun – over 9,000°F. Despite the intense heat, the crushing pressure keeps it solid. Scientists study seismic waves from earthquakes to understand what’s going on down there, which is how this study was conducted.
The inner core, located 3,000 miles (4,800 kilometers) below the Earth’s surface, was presumed to be a solid sphere. In the current study, scientists were primarily interested in understanding how the inner core rotates and in mapping its decelerating movement. They set out to explore why the inner core appeared to rotate at a rate slower than Earth’s rotation before speeding up again in 2010. To investigate, experts analyzed decades of seismic data, leading to their unexpected discovery that the surface of the inner core is changing shape.
In the analysis of multiple seismic waveforms, a particular set of data stood out as unusual. Further analysis of this data led to the conclusion that the Earth’s inner core is not solid but is able to change shape. The methodology was simple. Scientists leveraged seismic waveform data from various earthquakes that occurred between 1991 and 2024 near the South Sandwich Islands in Antarctica. Analysis of these waveforms revealed one dataset with unprecedented characteristics, hinting at physical upheavals inside the inner core.
The analysis of this extensive data set revealed a dynamic process previously unaccounted for in geological models. The seismic waveform data suggested that the inner core is dynamic and undergoing continuous and complex temporal reshaping. This challenges the notion of the inner core’s long-term stability. Researchers found that the inner core’s shallow boundary may undergo viscous deformation, gradually and repeatedly altering its shape due to intense pressures and interactions with the turbulent outer core.
Researchers noted that physical interactions between the inner and outer core seem to trigger these structural changes. The molten outer core, with its turbulence, was never before known to disrupt its inner counterpart within a human timescale. Now, however, it appears that the outer core is disturbing the inner core by forcing the deformation of its surface layer. This opens up a window to explore the previously hidden dynamics within Earth’s core.
Professor John Vidale, who led the research, believes that the edges of the inner core may have deformed by over 100 meters in some areas. “In all likelihood, this finding doesn’t affect our daily lives one iota, but we really want to understand what’s happening in the middle of the Earth,” said Professor Vidale.
This revelation has the power to improve our comprehension of Earth’s thermal and magnetic fields. It also sheds new light on the intricate interactions between the inner and outer core. According to researchers, it is possible that these changes are linked to alterations in Earth’s magnetic field. “The magnetic field has had jerks at various times in the past few decades, and we’d like to know if that is related to what we’re seeing at the inner core boundary,” said Professor Vidale.
A clearer understanding of these processes could refine our models of geomagnetic field generation, plate tectonics, and even the planet’s long-term climate stability.
This study not only challenges existing geological models but also reminds us that even the most fundamental aspects of our planet remain open to re-examination. The inner core – once thought to be a static, solid mass – appears to be in constant motion, changing and shape-shifting over time. Yet, many questions remain. What governs the pace of these changes? How do they influence the broader geodynamic processes of our planet? Could similar mechanisms be at play in the cores of other celestial bodies?
As technology advances and seismic data grows more precise, the inner depths of our planet will no longer be a distant enigma but a frontier waiting to be explored fully. The full study was published in the journal Nature Geoscience.
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