Earthquake-triggered submarine landslides in the St. Lawrence Estuary (Quebec, Canada) during the last two millennia and the record of the major 1663 CE M=7 event

In eastern Canada, the Charlevoix-Kamouraska/Bas-Saint-Laurent (CKBSL) seismic zone presents a seismic hazard almost as high as that of the active Pacific zone. The major event of February 5, 1663 CE, with an estimated magnitude of >= 7, highlights the importance of this seismic hazard. The numerous submarine landslides mapped in the St. Lawrence Estuary in the CKBSL seismic zone suggest that earthquakes triggered series of submarine slope failures. In this context, the SLIDE-2020 expedition on board the RV Coriolis II in the St. Lawrence Estuary aimed to map, image and sample more than 12 zones of submarine instabilities and their associated deposits. The analysis of sediment cores sampled in the distal sedimentary deposits from these landslides reveals the presence of rapidly deposited layers (turbidites, hyperpycnites and debrites) directly linked to the submarine landslides. Dating these land-slides with Pb-210 and C-14 techniques led to the identification of four periods of synchronous submarine landslides corresponding to the strongest historical earthquakes: 1663 CE, 1860/1870 CE, 1925 CE and 1988 CE (M >= 7, M = 6.1/6.6, M = 6.2, M = 5.9). This synchronicity over a distance reaching 220 km of several landslides supports a relationship between their triggering in the St. Lawrence Estuary and regional seismicity. The fact that as many as nine submarine landslides appear to have been triggered by the 1663 CE earthquake suggests that this event is the strongest recorded in the last two millennia in the region. (C) 2022 Elsevier Ltd. All rights reserved.

Automated summary

The Charlevoix-Kamouraska/Bas-Saint-Laurent (CKBSL) seismic zone in eastern Canada has a seismic hazard similar to that of the active Pacific zone. A major earthquake in 1663 triggered numerous submarine landslides in the St. Lawrence Estuary, indicating a relationship between earthquakes and submarine slope failures. Analysis of sediment cores and dating techniques revealed four periods of synchronous submarine landslides corresponding to strong historical earthquakes, with the event in 1663 being the most significant in the region in the past two millennia.