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Nat Geo
On the morning of November 11, just before 9:30 UT, a mysterious rumble rolled around the world.
The seismic waves began roughly 15 miles off the shores of Mayotte, a French island sandwiched between Africa and the northern tip of Madagascar. The waves buzzed across Africa, ringing sensors in Zambia, Kenya, and Ethiopia. They traversed vast oceans, humming across Chile, New Zealand, Canada, and even Hawaii nearly 11,000 miles away.
However, there was no big earthquake kicking off the recent slow waves. Adding to the weirdness, Mayotte's mystery waves are what scientists call monochromatic. Most earthquakes send out waves with a slew of different frequencies, but Mayotte's signal was a clean zigzag dominated by one type of wave that took a steady 17 seconds to repeat.
“I don't think I've seen anything like it,” says Göran Ekström, a seismologist at Columbia University who specializes in unusual earthquakes.
“It doesn't mean that, in the end, the cause of them is that exotic,” he notes. Yet many features of the waves are remarkably weird—from their surprisingly monotone, low-frequency “ring” to their global spread. And researchers are still chasing down the geologic conundrum.
It was just one week ago that France’s Bureau de Recherches Géologiques et Minières (BRGM), the geological agency for Mayotte, issued an updated report on the science behind a seismic swarm that’s been affecting the Indian Ocean island for more than six months.
And then, on Tuesday morning, came a jolting reminder that it’s not over yet, with a 5.1-magnitude earthquake at 8:11 a.m. local time. It was the largest since June 27, and the latest since the swarm began on May 10, creating hundreds of small and frequent quakes – and a few larger ones.
M 5.0 - 6km SSE of Pamandzi, Mayotte
We present SKS splitting measurements in the Western Indian Ocean, recorded on 20 land and 57 seafloor seismometers deployed by the RHUM-RUM experiment (Réunion Hotspot and Upper Mantle – Réunions Unterer Mantel). We discuss our splitting observations within their geodynamic settings and compare them to SKS splitting parameters predicted from an azimuthally anisotropic Rayleigh wave tomography model that includes the RHUM-RUM data. We find that anisotropic directions poorly correlate with the present-day motion of the Somali plate, which at [less than symbol]2.6 cm/yr may be too slow to cause strongly sheared fabric in the asthenosphere.
originally posted by: angelchemuel
Pilot Whales beached themselves in NZ earlier this week, just like they did in Japan a week before Fukushima. I tend to find there tends to be an EQ within the week after Pilots do this....not scientific of course.....
Rainbows
Jane
originally posted by: charlyv
So... the major contender would be a meteor strike in the deep ocean. They must be working this out.
originally posted by: angelchemuel
Pilot Whales beached themselves in NZ earlier this week, just like they did in Japan a week before Fukushima. I tend to find there tends to be an EQ within the week after Pilots do this....not scientific of course.....
Rainbows
Jane