SCIENCE
Deep below Earth’s surface, a pulse ticks every 26 seconds—unfelt, but unmistakable.
By Aniket Chakraborty
June 4, 2025
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First recorded in the 1960s, this quiet tremor has echoed unchanged for decades.
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Known as a "microseism", it was initially traced to the equatorial Atlantic Ocean.
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In 2005, digital seismic data revived the mystery and pointed to the Gulf of Guinea.
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One theory blames powerful ocean waves striking the continental shelf.
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Another suspects underwater volcanic activity near São Tomé Island.
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Despite years of study, there’s still no definitive answer to what causes it.
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Some scientists have deprioritized it—yet it continues, steady and unexplained.
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Every 26 seconds, Earth ticks like a geologic metronome in the deep.
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A silent heartbeat beneath the waves—unresolved, uncanny, and still counting.
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