A new study has uncovered that even the slightest stress can set off tidally triggered earthquakes.
Years ago, scientists realized that earthquakes along with mid-ocean ridges and underwater mountain ranges at the edges of the tectonic plates are linked with the tides. But nobody could figure out why there's an uptick in tremors during low tides.
Seismologist and co-lead of the study Christopher Scholz said, everyone was sort of stumped because according to conventional theory, those earthquakes should occur at high tides.
In a study published in the Journal of Nature Communications, researchers have uncovered the mechanism for this seeming paradox, and it comes down to the magma below the mid-ocean ridges.
Scholz said, it's the magma chamber breathing, expanding, and contracting due to the tides, that's making the faults move. During movement, the upper block slides down with respect to the lower one. So, scientists expected that at high tides, when there is more water sitting on top of the fault, it would push the upper block down and cause earthquakes. But that's not what happens. Instead, the fault slips down during low tide, when forces are actually pulling upwards which is the opposite of what you'd expect.
Because the volcano erupts every ten years or so, scientists have set up dense networks of ocean bottom instruments to monitor it. The team used the data from those instruments to model and explore different ways the low tides could be causing the tremors.
In the end, it came down to a component that no one else had considered before, the volcano's magma chamber, a soft, pressurized pocket below the surface. The team realized that when the tide is low, there is less water sitting on top of the chamber, so it expands. As it puffs up, it strains the rocks around it, forcing the lower block to slide up the fault, and causing earthquakes in the process.
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