Earthquake Geology is crucial to understanding fault dynamics, crustal deformation, and morphotectonics of seismogenic mountain ranges. Characterizing Himalayan active faults remains challenging due to infrequent great earthquakes, insufficient paleo- earthquake knowledge, and prolonged erosion/sedimentation precluding cumulative scarps, making examining the earthquake behavior over multiple seismic cycles strenuous. Techniques like characterizing the inter-, co-, and post-seismic periods, revealing concealed structures, etc., contribute to a more thorough grasp of the tectonic processes from seconds to decadal scales. Thus, an integrated approach to paleoseismology, seismology, geodesy, and geophysics helps identify active structures and understand a fault'sslipbehavior, which is essential for constraining possible earthquakes' magnitude and recurrence. This session invites a broad range of interdisciplinary contributions addressing recent or past intracontinental earthquakes and modeling of active faults, which would enhance our understanding of fault mechanics and

the earthquake cycle.