Because seismogenic faults are typically buried at great depth, high spatial resolution observations of interactions between slow slip, fast slip, and...

Slip on faults occurs as a spectrum ranging from continuous sliding, where motion is too slow to radiate seismic waves (aseismic creep), to rapid move...

With ever-improving geophysical observations, how do we better understand large earthquakes in the past and foretell their potential behavior in the f...

In this talk, Joanna L. Dyl, Ph.D., will discuss recurrent patterns across the history of major earthquakes in the San Francisco Bay Area, focusing on...

We continue to gradually improve upon the current suite of near-real-time USGS earthquake information systems and products that provide estimates of t...

Identifying and characterizing cryptic, distributed faulting in high-relief topography can be challenging due to vegetative cover and high rates of hi...

In this talk, a framework for modeling the effects of disasters on households' well-being will be presented. The framework extends traditional seismic...

In some subduction zones, the plate boundary fault slips at rates faster than tectonic plate rates, but orders of magnitude slower than typical earthq...

Recent results from an EGS project in Finland suggest a possibly successful physics-based approach in controlling stimulation-induced seismicity in ge...

Ecuador, located in South America, is roughly the size of Nevada, but is very active geologically. There are 84 Quaternary volcanoes, and three large ...