“…Over the last decades, several outcrop studies focusing on the internal architecture of MTDs have been undertaken in order to investigate processes occurring during the transport and emplacement of the failed material. These studies, which have mostly been carried out in siliciclastic systems and only rarely in carbonate systems (Pickering, ; Lucente & Pini, ; Pickering & Corregidor, ; Van Der Merwe et al ., , ; Butler & McCaffrey, ; Ogata et al ., ), indicate that MTDs move along a basal detachment surface that may either follow the bedding plane (Strachan, ; Van Der Merwe et al ., ) or plough through the underlying beds incorporating the underlying material into the moving mass (Strachan, ; Ogata et al ., ; Sobiesiak et al ., ). Internally, gravity‐driven soft‐sediment deformation processes result in the formation of an array of structures including dip‐slip and oblique‐slip normal faults (Alsop & Marco, ), extensional sedimentary fissures in the upper extensional head (Winterer et al ., ; Strachan, ; Spalluto et al, ), and folds, thrusts, ramps and erosional surfaces in the lower compressional part.…”