Three decades of geodetic monitoring have established slow slip events (SSEs) as a
common mode of fault slip, sometimes linked with earthquake swarms and in a few cases …

Earth's crust is continuously subjected to oscillatory stress perturbations due to the solid
Earth and ocean tides. The seismic response to such stress modulations carries information …

Swarms are bursts of earthquakes without an obvious mainshock. Some have been
observed to be associated with transient aseismic fault slip, while others are thought to be …

In Nepal, after every large earthquake, local people appear to be motivated to get better
prepared for future earthquakes. However, their motivation vanishes before effective …

The frictional properties of faults control the initiation and propagation of earthquakes and
the associated hazards. Although the ambient temperature and instantaneous slip velocity …

The seismometer deployed by the InSight lander measured the seismic velocity of the
Martian crust. We use a rock physics model to interpret those velocities and constrain …

Purpose: Prigi Beach has the largest fishing port in East Java, but the topography of this
beach is quite gentle, so it is prone to disasters such as tidal flooding. The tides of seawater …

Seismicity rate is sometimes observed to correlate with periodic stress oscillations, such as
seasonal changes in hydrological loads, or solid-earth and oceanic tidal stresses. However …

The role of solid Earth tide in fault reactivation has significant implications for understanding
earthquake triggering, carbon sequestration, and the global carbon budget. Despite …

Deformation mechanisms of glaciers are highly sensitive to basal temperature; the motion of
temperate glaciers is dominated by basal slip while cold‐based glaciers deform mainly by …