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Scientists have not seen a metal volcano erupt on another world. Instead, a large-scale laboratory experiment offers a glimpse of what one might look like: metallic melt moved much faster than silicate lava and formed thin, braided channels that could leave distinctive surface patterns. Those patterns are possible clues for future planetary studies—not evidence that metal volcanoes have been found on an asteroid.

What is ferrovolcanism?

Ferrovolcanism is a predicted form of volcanism involving molten metal. It is an unusual idea because familiar volcanoes erupt silicate rock, while some planetary bodies may contain metal-rich material that could melt and flow. Arianna Soldati and coauthors described ferrovolcanism as “yet to be directly observed” in their 2021 paper in Nature Communications.

The study, “Imagining and constraining ferrovolcanic eruptions and landscapes through large-scale experiments,” was published on March 17, 2021, in Nature Communications, volume 12, article 1711. Read the paper.

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What did the lava-flow experiment show?

At the Syracuse University Lava Project, researchers conducted large-scale experiments with metallic and silicate flows. Under the tested conditions, the metallic melt was denser and less viscous than the silicate lava, and it traveled about ten times faster. In one documented experimental flow, the measured speeds were approximately 0.41 meters per second for the metal and 0.04 meters per second for the silicate. These are laboratory measurements, not predictions of how fast lava would move on an asteroid.

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The two materials did not simply mix into one flow. The metallic melt was largely decoupled from the silicate: it traveled mainly through braided channels beneath the silicate flow, then emerged near the silicate flow’s front. The Syracuse University Lava Project lists the study among its research publications. See the project’s publications.

How might metal flows differ from familiar lava?

Feature Silicate flow Metallic flow in the experiment
Material behavior Less dense and more viscous than the metallic melt in the tested conditions. Denser and less viscous than the silicate lava in the tested conditions.
Relative speed About 0.04 m/s in one documented laboratory flow. About 0.41 m/s in that same documented laboratory flow; the study reports metal moving about ten times faster under its tested conditions.
Flow pattern Thicker, more compact flow in the comparison described by the researchers. Thin, low-relief braided channels, largely beneath the silicate flow and breaking out near its front.
Evidence status Observed in the laboratory experiment. Observed in the laboratory experiment; proposed planetary landforms remain hypothetical.

The experiments suggest that metal-rich eruptions could leave thinner, lower-relief and more braided features than familiar silicate flows. If similar features were identified on a planetary surface, they might help scientists investigate whether metallic melt had once moved there. A resemblance alone would not establish that an eruption occurred.

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Could 16 Psyche have metal volcanoes?

Asteroid 16 Psyche is relevant to the hypothesis because it is metal-rich. NASA’s Jet Propulsion Laboratory describes the Psyche mission as studying an asteroid whose surface contains substantial metal, with the goal of improving understanding of iron cores and planet formation. Learn about NASA’s Psyche mission.

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That context makes Psyche a body of interest; it does not confirm ancient volcanoes there. The 2021 experiments show how metal and silicate behaved in a particular laboratory setup. Applying those results to another world requires assumptions about its materials, gravity, temperatures and surface conditions. The study did not observe an alien eruption or establish that Psyche—or any other planetary body—has ferrovolcanic features.

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What would an eruption on another world look like?

The experiment offers a physical basis for one possible answer: a fast-moving metallic component could travel in braided channels, partly hidden beneath silicate lava, and emerge near the flow’s leading edge. Such a process might leave thin, branching or braided patterns rather than the thicker, more compact shapes associated with familiar silicate flows.

Those are hypotheses about what researchers might look for, not a description of a confirmed landscape. Ferrovolcanism remains predicted and unobserved directly. The experiment narrows possibilities by showing how these materials flowed under tested conditions, while observations of planetary surfaces would be needed to assess whether any candidate features fit the idea.

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