Figure 4. Coseismic Interferograms of the 24 February 2004 Al Hoceima earthquake. Each fringe shows 2.83 cm of surface displacement along the radar line of sight. Dashed lines are digitized fringes used in modeling the interferograms. Blue line is the best model fault. Barbed lines are inactive thrust faults shown to facilitate comparison of the interferograms. Black arrows indicate radar look direction.