Li-Chieh Lin, UCR: We have combined InSAR from Sentinel-1 and UAVSAR over the creeping segment of the central San Andreas fault to make a map of surface deformation velocities in 3D! This allows us to map the surface creep along the fault with minimal assumptions! Come to our poster (#086)!

Ahmed Elbanna, Illinois: What is the range of spatial and temporal scales we need to understand in earthquake dynamics. About 15 orders of magnitude in time, and 12 in space! And each process at a particular scale affects the others at other scales – we need to understand them all!