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The Union Ecuador/south Colombia convergent margin is affected past recurrent subduction earthquakes with magnitudes > 7.5, wish the 1906, 1942, 1958, 1979 and 2016 events. The subduction encroach is defined past the twist of the Esmeraldas Turbidite System (ETS) fed by the large Esmeraldas Canyon that deeply incises the landmass pitch and that connects straight land with the Esmeraldas River. The elaborated description of cores collected indium the left-hand (western) proximal levee of the ETS and in two lobes allowed discriminating II types of coarse-grained deposits: (1) “classical” flood-generated turbidites ar normally hierarchal beds with structureless, laminated and cross-laminated intervals and high organic-count content, patc (2) quake -induced deposits consist of intermingled ordinarily -hierarchal laminated/cross-laminated intervals distributed by erosive surfaces. These latter ar taken to be deposited by quasi-synchronous flows generated during a one seism. Organic matter is absent indium such beds patc ferromagnesian minerals and pumices are exuberant, suggesting remobilization of the incline deposits. When two amalgamated beds are superimposed, the interbedded compact time interval is non bioturbated, suggesting a short-circuit time period between the beds deposition, safe dating verification and olibanum the impact of vitamin A John Major earthquake traumatize and following earthquakes on the triggering of landslides.