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American Focus > Blog > Tech and Science > Solid Rock Caught Flowing 1,700 Miles Beneath Surface in Experimental First : ScienceAlert
Tech and Science

Solid Rock Caught Flowing 1,700 Miles Beneath Surface in Experimental First : ScienceAlert

Last updated: June 17, 2025 3:25 pm
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Solid Rock Caught Flowing 1,700 Miles Beneath Surface in Experimental First : ScienceAlert
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The Mystery of Earth’s D” Layer Unraveled: Solid Rock Flows Deep Below

For decades, scientists have been puzzled by the D” layer, located some 2,700 kilometers below the Earth’s surface. Recent research may have finally shed light on the enigmatic zone – it appears that solid rock is flowing deep within the Earth.

Seismic waves passing through the D” layer unexpectedly accelerate, indicating that something unique is happening at this boundary. A study in 2004 suggested that extreme pressures and temperatures could transform the mineral perovskite into a different phase known as ‘post-perovskite’ near the D” layer boundary.

However, further investigations revealed that this new phase alone could not account for the increased speed of seismic waves. In a new study, researchers from Switzerland and Japan conducted simulations and experiments, demonstrating that the alignment of crystals in post-perovskite is crucial for the acceleration of seismic waves.

Earth layers
Perovskite turns into post-perovskite near the core. (ETH Zurich)

Lead researcher Motohiko Murakami from ETH Zurich stated, “This discovery not only solves the mystery of the D” layer but also opens a window into the dynamics deep within the Earth. We have finally found the last piece of the puzzle.”

The team recreated Earth’s deep layers in the lab and discovered that the alignment of post-perovskite crystals determines its hardness, affecting the propagation of seismic waves. They also observed a convection pattern in the solid rock above the D” layer, driven by the movement of cooler and hotter materials, influencing crystal alignment.

Rock alignment
Convection above the D” layer controls crystal alignment. (ETH Zurich)

The researchers concluded that the texture of the post-perovskite phase explains key features of the D” discontinuity, enhancing our understanding of Earth’s complex processes involving heat, pressure, and movement. This knowledge is crucial for interpreting phenomena such as volcanic eruptions and the Earth’s magnetic field.

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The core-mantle boundary (CMB) where the solid mantle meets the liquid outer core is a significant area of interest, marking a transition between materials with distinct properties. Murakami emphasized, “Our discovery shows that the Earth is not only active on the surface but also in motion deep inside.”

While this study resolves some mysteries, many questions remain about the deep layers of the Earth. The findings have been published in Communications Earth & Environment.

TAGGED:BeneathCaughtExperimentalFlowingMilesRockScienceAlertSolidSurface
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