Numerical Modelling of Late Pleistocene to Holocene Earthquake‐Induced Progressive Rock Slope Damage in the Paraglacial Serpentine Valley, Prince William Sound, Alaska
Landslides in deglaciating fjords pose a potential tsunami threat to nearby communities; however, processes contributing to long‐term progressive rock damage and landslide conditioning remain poorly constrained in paraglacial settings. Here, we analyse the role of earthquake‐induced rock mass damage over late Pleisto...