Oscillations in stress, such as those created by earthquakes, can increase permeability and
fluid mobility in geologic media. In natural systems, strain amplitudes as small as 10− 6 can …

For ten earthquakes in nonmagmatic settings, there are credible published accounts of pre-
earthquake deformation-rate changes lasting hundreds of seconds to more than a decade …

One of the fundamental questions of ecology is what controls biodiversity. Recent theory
suggests that biodiversity is controlled predominantly by neutral drift of species …

Injecting fluids in the crust, or their extraction, changes pore pressure and poroelastic
stresses. Both pressure and stress changes can promote seismicity and, hence, the seismic …

In late August 2005, a swarm of more than a thousand earthquakes between magnitudes 1
and 5.1 occurred at the Obsidian Buttes, near the southern San Andreas Fault. This swarm …

Geofluids (2010) 10, 206–216 Abstract Hydrologic responses to earthquakes, including
liquefaction, changes in stream and spring discharge, changes in the properties of …

We analyze the co-seismic groundwater level responses to four great earthquakes recorded
by China's network of groundwater monitoring wells. The large number of operational wells …

The Endeavour segment of the Juan de Fuca ridge is host to one of the most vigorous
hydrothermal areas found on the global mid-ocean-ridge system, with five separate vent …

Earth's porous crust and the fluids within it are intimately linked through their mechanical
effects on each other. This paper presents an overview of such" hydromechanical" coupling …

Key questions in fault reactivation in shales relate to the potential for enhanced fluid
transport through previously low‐permeability aseismic formations. Here we explore the …