LASER-INTERFEROMETRIC SEISMOACOUSTIC OBSERVATORY (LISO)

Strong asperities nucleate earthquakes on laboratory faults

Dense Seismic Recordings of the 2023 Kahramanmaraş Earthquake Sequence in Southeastern Türkiye

Mapping 3D Sedimentary Structures with Joint Inversion of H/V Spectral Ratios and Multimode Dispersion Curves Derived from Ambient Noise—Application to the Xiong‘an New Area, China

Investigation of the main drivers influencing sediment property change and coastal erosion in Central Vietnam

Fast Probabilistic Seismic Hazard Analysis Through Adaptive Importance Sampling

Paleoseismology of the Zia Fault and Its Impact on Seismic Hazard for Albuquerque, New Mexico, USA

Developing a Probabilistic Tsunami Hazard Assessment Framework for Pacific Sources: USGS Powell Center Meeting Summary

Natural Hazard Risk Assessments Applicable to Enterprise Risk Management

Detection of a Permeable Aquifer Geohazard Above Potash Mines using In-mine Time-domain Electromagnetics

Geological evidence for repeated slip-to-the-trench style megathrust earthquakes at the Japan Trench

Weak, frictionally unstable input sediments explain shallow seismogenesis at the north Sumatran subduction zone

Coal Mine Hidden Disaster Detection Based on Opposing Coils Transient Electromagnetic Method

Aseismic creep and strain partitioning accommodating the Nubia-Eurasia oblique convergence in northern Africa from InSAR analysis

Leveraging Submarine DAS Arrays for Offshore Earthquake Early Warning: A Case Study in Monterey Bay, California

Applying the ETAS Model to Simulate Earthquake Sequences for Hazard Assessment in Crustal Seismicity Regions with Scarce Data

Determination of Ground Subsidence Around Snow Fences in the Arctic Region

Propagation Characteristics of Tsunamis in an Atmosphere‐Ocean Coupled System Revealed by Wave Gradiometry: The 2022 Hunga Tonga–Hunga Ha’apai Eruption Case

Law of overburden and surface deformation in roof cutting and backfilling mining under thin bedrock in shallow buried coal seam

Combining Multisite Tsunami and Deformation Modeling to Constrain Slip Distributions for the 1700 C.E. Cascadia Earthquake