Insights into tectonic hazards since the 2004 Indian Ocean earthquake and tsunami
In 2004, an earthquake of moment magnitude Mw 9.1–9.3 ruptured over 1,500 km of the Sunda megathrust under the Indian Ocean, produ…
In 2004, an earthquake of moment magnitude Mw 9.1–9.3 ruptured over 1,500 km of the Sunda megathrust under the Indian Ocean, produ…
Megathrusts, faults at the plate interface in subduction zones, exhibit substantial spatiotemporal variability in their slip behaviour. Many previo…
Forecasting the onset, evolution and end of volcanic eruptions relies on interpretation of monitoring data—particularly seismic signals, such as …
Quantitative estimates of magma storage are fundamental to evaluating volcanic dynamics and hazards. Yet our understanding of subvolcanic magmatic …
The inner core has been inferred to change its rotation rate or shape over years to decades since the discovery of temporal variability in seismic …
Turbidity currents carve Earth’s deepest canyons, form Earth’s largest sediment deposits, and break seabed telecommunications cables. Directly …
Strong earthquakes in mountain landscapes can trigger widespread slope failures, initiating chains of multiple hydro-geomorphic hazards. These impa…