Tides in Earth’s crust trigger small, deep quakes

Study of one portion of the San Andreas fault finds that just a little added stress makes a quake more likely

The subtle changes in stress caused by tides in Earth’s crust can trigger small, deep quakes along a seismically active portion of California’s San Andreas fault, a new analysis suggests.

The same forces of attraction that cause ocean tides also cause tides in Earth’s rocks, says Amanda Thomas, a seismologist at the University of California, Berkeley.