When we think of earthquakes, we imagine sudden, violent shaking. But deep beneath Earth’s surface, some faults move in near silence. These slow, shuffling slips and their accompanying hum—called tremors—don’t shake buildings or make headlines. But scientists believe they can serve as useful analogs of how major earthquakes begin and behave.
A ripple effect: Minor quakes can disrupt natural tectonic patterns deep underground and change stress landscape
