Slip faults, particularly strike-slip faults, can indeed generate large tsunamis, contrary to previous beliefs. The discussion highlights the concept of "supershear," where slip velocity exceeds S-wave speed but remains below P-wave speed. The San Andreas Fault and Gulf of Aqaba are identified as high-risk areas for tsunami generation, while the mid-Atlantic Ridge, characterized by spreading rather than lateral movement, is less likely to produce similar events. Transform faults exist within the mid-Atlantic Ridge, but their geometry may not favor tsunami generation as effectively as faults in the Pacific. Understanding these dynamics is crucial for assessing tsunami risks associated with different fault types.