Earth Shaken Every 90 Seconds for Nine Days: Scientists Uncover Baffling Phenomenon


For nine days in late 2024, our planet pulsed like a heartbeat. Every 90 seconds, a seismic tremor rippled through Earth’s crust—a rhythmic shaking so precise it left scientists stunned. Detected by thousands of monitoring stations worldwide, the tremors were too faint for humans to feel but revealed an unprecedented geological mystery unfolding beneath our feet.

The event began abruptly on November 5th. Seismologists initially scrambled to rule out technical glitches, only to confirm the signals were real. Dr. Lin Mei of the Global Seismology Institute described it as "nature’s metronome," adding, "We’ve seen volcanic tremors and earthquake swarms, but never a global pattern this regular. It defied all our models."

The Underwater Volcano Connection

Evidence quickly pointed to an oceanic origin. Satellites detected thermal anomalies near Mayotte, a French island between Mozambique and Madagascar, where a massive undersea volcano has been active since 2018. Researchers theorize the tremors stemmed from "magma chamber collapses"—repeated implosions as molten rock drained from an underground reservoir, causing the seafloor to shudder like an emptying balloon.

Dive deeper into the science behind these tremors with exclusive visuals and expert analysis in this groundbreaking report.

Why It Matters

Beyond its eerie rhythm, the event offers invaluable insights. Dr. Kenji Tanaka of Kyoto University notes, "These tremors are a live feed into Earth’s plumbing. Understanding them could revolutionize tsunami prediction." Indeed, the Mayotte volcano—now one of Earth’s largest—remains active, with seismic whispers still echoing months later.

While the pulsing ceased on November 14th, its legacy endures. As robotic submersibles map the seafloor’s new topography, one truth is clear: Earth still guards epic secrets. For nine days, it drummed a warning—and scientists are finally learning to listen.


Image: Simulation of magma movement beneath Mayotte’s seabed / Credit: CNRS-IPGP

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