Seismic sensors first picked up the event originating near an island between Madagascar and Africa. Then, alarm bells started ringing as far as Chile, New Zealand and Canada.
Hawaii, almost exactly on the other side of the planet, also picked up the 'event'.
Nobody knows what it was.
Meteorite? Submarine volcano? Nuclear test?
"I do not think I've seen anything like that," National Geographic reports Colombian University seismologist Göran Ekström as saying. "It does not mean that, in the end, the cause of them is that exotic."
At the center of the mystery is the tiny island of Mayotte, positioned about half way between Africa and Madigascar. It has been subjected to a swarm of earthquakes since May. Most were minor, but the largest – on May 8 – was the largest in recorded history of the island, topping magnitude 5.8.
But the earthquake swarm was in decline before the mysterious ringing was detected earlier this month.
Ekström, who specializes in unusual earthquakes, points out much about the November 11 event was weird. It was as though the planet rang like a bell, maintaining a low-frequency monotone as it spread.
Earthquakes, by their very nature, usually register as short-sharp 'cracks'. As tensions in the Earth's crust suddenly release, the pulses of clearly identified seismic waves radiate outward from where the slippage occurs.
The first signal is called a primary wave: high-frequency compression waves that radiate in bunches.
Then comes a secondary wave: these high-frequency waves tend to 'wiggle' somewhat more.
Only then comes the surface waves: these slow, deep rumbles tend to linger, and can circle the Earth several times.
The November 11 event is notable in that no primary or secondary waves were detected.
All that was registered was the deep, resonating surface wave. And it did not 'rumble' as a earthquake's surface wave tends to. Instead, it kept a lot of cleaner – almost musical – frequency.
National Geographic reports that French Geological Survey suspects a new volcano may develop off the coast of Mayotte. While the island was created by volcanic activity, it has been dormant for more than 4000 years.
The French believe the weird ringing may have been generated by a magma movement some 50km off the coast and under deep water. This is supported by GPS sensors detecting Mayotte has moved some 5cm to the southwest for less than five months.
But it's a poorly mapped region. Exactly what's beneath the ocean can only be guessed at.
Ekström believes that the unusually pure signal could have been caused by magma sloshing about inside a chamber, or being forced through a gap in the suburface rocks.
But he's not sure.