Although the magnitude 8.7 Nias-Simeulue earthquake of March 28, 2005, was technically an aftershock, the temblor nevertheless killed more than 2,000 people in an area that had been devastated just three months earlier by the December 2004, magnitude 9.1 earthquake. Now, data returned from instruments in the field provide constraints on the behavior of dangerous faults in subduction zones, fueling a new understanding of basic mechanics controlling slip on faults, and in turn, improved estimates of regional seismic risk.