▪ Abstract Earthquake triggering is the process by which stress changes associated with an
earthquake can induce or retard seismic activity in the surrounding region or trigger other …

It has been known for a long time that slip accompanying earthquakes accounts for only a
fraction of plate tectonic displacements. However, only recently has a fuller spectrum of …

Earthquakes occur as a result of global plate motion. However, this simple picture is far from
complete. Some plate boundaries glide past each other smoothly, while others are …

Large, sustained well water level changes (> 10 cm) in response to distant (more than
hundreds of kilometers) earthquakes have proven enigmatic for over 30 years. Here we use …

Abstract The 1992 magnitude 7.3 Landers earthquake triggered an exceptional number of
additional earthquakes within California and as far north as Yellowstone and Montana …

Abstract Approximately 0.4% of explosive volcanic eruptions occur within a few days of
large, distant earthquakes. This many “triggered” eruptions is much greater than expected by …

Earthquake-induced crustal deformation and ground shaking can alter stream flow and
water levels in wells through consolidation of surficial deposits, fracturing of solid rocks …

In this introduction, we review much of the recent work related to stress transfer, earthquake
triggering, and time‐dependent seismic hazard in order to provide context for the special …

Space–time anomalies of Earth's emitted radiation in the thermal infrared spectral range
(TIR) measured from satellite months to weeks before the occurrence of earthquakes, have …

Regional‐scale triggering of local earthquakes in the crust by seismic waves from distant
main shocks has now been robustly documented for over a decade. Some of the most …