The Mayotte vibrations took about 40 minutes to reach Britain, and an hour and 15 minutes to reach Hawaii, more than 11,000 miles from their point of origin.
Such low frequency rumbles are rare but not unheard of. Scientists have detected them before after glacier calving, landslides and sudden shifts of magma beneath volcanoes. There are no glaciers near Mayotte and an underwater landslide would have been picked up by hydrophones in the surrounding ocean, said Hicks. That leaves a magma shift somewhere under the seabed as the prime culprit.
Hicks believes magma may suddenly have drained from a volcanic chamber about 10 miles under the seafloor near Mayotte, setting off the deep rumble that spread around the world. While strong enough to be picked up by sensitive seismometers, the vibrations would have been minuscule: far smaller than a millimetre. “It’s something that you wouldn’t perceive,” he said.
Pierre Briole, a geoscientist at École Normale Supérieure in Paris, has reached a similar conclusion. He believes that a third of a cubic mile of magma may have drained from a volcanic chamber under the seafloor, unleashing deep vibrations when its roof collapsed.
Much of the seismic sleuthing played out on social media with professional and amateur scientists working together. “Overall, a fascinating demonstration of open science on Twitter and engagement between scientists and citizen seismologists,” said Hicks.
https://www.theguardian.com/science/2018/nov/30/magma-shift-mysterious-seismic-wave-event-mayotte?CMP=fb_gu&fbclid=IwAR2tSyVv99SeJVXVLam82rx16EiV0umhot_FbJ7OOowqTnlxqXoeZ-h69pA