In tectonically active regions, the movement of the Earth's crust not only generates earthquakes but riddles the subsurface with cracks and fractures lined with highly reactive rock surfaces containing many imperfections, or defects. Water can then filter down and react with these defects on the newly fractured rock. In the laboratory, Masters student Jordan Stone simulated these conditions by crushing granite, basalt and peridotite -- rock types that would have been present in the early Earth's crust. These were then added to water under well controlled oxygen-free conditions at varying temperatures.