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This decade will likely be regarded in the geosciences as a time of an unprecedented explosion of fault zone drilling projects. The past few years have seen the initiation of proj-ects including the Nojima Fault Drilling, San Andreas Fault Observatory at Depth (SAFOD), the Taiwan Chelungpu Fault Drilling Project (TCDP), the Gulf of Corinth Rift Laboratory (CRL) on land, and the Nankai Trough Seismogenic Zone Experiment (NanTroSEIZE) and Costa Rica Seismogenesis Project (CRISP) at sea (see Table 1 for references).Each of these projects has unique objectives and scientific drivers, yet they share the fundamental goal of seeking direct access to zones of active faulting, particularly ones that generate earthquakes or have hosted seismic slip. This burgeoning interest in active fault drilling is taking place in the context of very rapidly growing research efforts on the mechanics and dynamics of faulting processes, integrating rock mechanics, seismology, geodesy, frictional physics, and fluid-fault interactions. There is a widespread recognition that our science lacks an integrated theory and understand-ing of the fundamental processes governing earthquakes and fault behavior, and the factors that control their natural variability.On 23–26 May 2006, eighty scientists and engineers from around the world gathered for the

Joint IODP-ICDP Workshop Examines Challenges of Fault Zone Drilling