The Emerald Isle has far fewer earthquakes than neighboring Britain. Now scientists think they know why.
© NASAIreland and Britain sit thousands of kilometers from the nearest tectonic plate boundary and just a few dozen from each other, yet Britain experiences far more earthquakes than Ireland.
Ireland and Britain should be, seismologically speaking, equally boring. The two islands lie thousands of kilometers from the nearest plate boundary and are not volcanic hot spots. But though the ground rarely rumbles in Ireland, neighboring Britain experiences plenty of weak and moderate earthquakes.
The
lithosphere — Earth's outermost rocky veneer, which includes the crust and the solid upper mantle — is thicker and cooler beneath Ireland than it is beneath Britain, new research has suggested. Cool, thick lithosphere is mechanically stronger than warm, thin lithosphere, which could explain the Emerald Isle's puzzling paucity of earthquakes. The
new results, published in
Geophysical Journal International,
hinted that lithosphere thickness could underpin patterns in seismic activity in other places far from plate boundaries.
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