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A massive sensitive clay landslide, Quyon Valley, southwestern Quebec, Canada, and evidence for a paleoearthquake triggering mechanism
Abstract
A landslide debris field covering ~ 31 km 2, the presence of large sediment blocks up to hundreds of meters long, and the exposure of deposits of a single landslide along the incised course of the Quyon River are evidence of a massive failure of sensitive Champlain Sea glaciomarine sediments along the lower Quyon Valley, southwestern Quebec, Canada. Seventeen radiocarbon ages indicate that the failure occurred between 980 and 1060 cal yr BP. Twenty-four additional radiocarbon ages reveal that nine landslides within a 65-km belt in the Quyon"Ottawa area also occurred at approximately this time. In combination, the contemporaneous occurrence of ten landslides between 980 and 1060 cal yr BP, the setting or morphology of five of the other failures, and the close proximity of two of the failures to the Quyon Valley landslide provide circumstantial evidence of a paleoearthquake-triggering mechanism. The paleoearthquake is estimated to be Mw ~ 6.1 or larger, with the epicenter within the West Quebec Seismic Zone. A common earthquake-triggering mechanism for the three largest landslides in eastern Canada suggests a close link between massive failures of sensitive glaciomarine sediments and the regional seismicity.
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The surficial deposits of the Ottawa-Bonnechere Graben consist of glacial, fluvial, and marine sediments dating back 10000-12000 years.
“The surficial deposits of the OBG consist of glacial, fluvial, and marine sediments (Brooks 2013) that date back 10000 -12000 years (Russell et al. 2011).”
From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Brooks 2013
Evidence of palaeoseismicity has been identified on quick clay deposits related to landslides in the OBG.
“Given the scarcity of surface ruptures, evidence of palaeoseismicity had been identified on quick clay deposits related to landslides in the OBG”
From Tectonic geomorphology of the Ottawa-Bonnechere Graben, Eastern Canada: implications for regional uplift and intraplate seismicity (2023) · cites this paper as Brooks 2013
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Cited by
Sorted by citations
Gusti, U. K., Peace, A. L., & Rimando, J. (2023) · Canadian Journal of Earth Sciences · doi:10.1139/cjes-2022-0137 · Cited by 7
Metadata
- Authors
- Brooks, G. R.
- Venue
- Quaternary Research
- Publisher
- Cambridge University Press (CUP)
- Published
- 2013-11
- Volume
- 80
- Issue
- 3
- Pages
- 425-434
- ISSN
- 0033-5894
- 1096-0287
- Cited by
- 29
- References
- 0
- Language
- en
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