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TitleSouthwind Fiord, Baffin Island, Nunavut: a natural laboratory to explore modern turbidity currents, submarine landslides and iceberg scouring in an Arctic environment
 
AuthorNormandeau, AORCID logo; Mackillop, K; Macquarrie, M; Philibert, G; Bennett, R
SourceCanada-Nunavut Geoscience Office, Summary of Activities 2020, 2021 p. 81-91 Open Access logo Open Access
LinksOnline - En ligne
Image
Year2021
Alt SeriesNatural Resources Canada, Contribution Series 20200643
PublisherCanada-Nunavut Geoscience Office
Documentserial
Lang.English
Mediapaper; on-line; digital
File formatpdf
ProvinceNunavut
NTS16L/09; 16L/16
AreaSouthwind Fiord; Baffin Island
Lat/Long WENS -62.5000 -62.0000 67.0000 66.6167
Subjectsmarine geology; surficial geology/geomorphology; sedimentology; geophysics; Nature and Environment; Science and Technology; Health and Safety; continental margins; marine environments; fiords; marine sediments; turbidity currents; landslides; mass wasting; landslide deposits; slope stability analyses; slope failures; icebergs; scouring; depositional environment; depositional history; erosion; bedforms; geophysical surveys; acoustic surveys, marine; marine sediment cores; core analysis; grab samples; currents; conductivity; temperature; bathymetry; water analyses; geophysical logging; Arctic; Infrastructures
Illustrationslocation maps; geoscientific sketch maps; schematic representations; photographs; geophysical profiles; time series; geophysical logs; geophysical images; plots
ProgramPublic Safety Geoscience Baffin Bay
ProgramProgram of Energy Research and Development (PERD)
Released2021 03 01
AbstractThe Geological Survey of Canada has a long history of regional assessment of marine geohazards in Arctic environments. Regional mapping allows identification of the distribution of hazards on the seafloor and is a critical part of hazard assessments. However, it does not shed light on understanding the recurrence and triggers of marine geohazards because it consists of one static view of the seafloor. In order to better understand the dynamic nature of seafloor environments, an experiment in Southwind Fiord, Nunavut began by monitoring and recording active marine geohazards. The preliminary data allowed recording of the effect of active turbidity currents and iceberg groundings in the fiord. Both these processes have led to erosion and deposition of sediment on the seafloor. A submarine landslide recorded in the fiord in 2018 appeared to have been triggered by an iceberg grounding on the fiord slope. A submarine landslide triggered by iceberg grounding is a significant discovery, as icebergs ground in many fiords and across the continental margin of Baffin Bay, therefore representing a previously unknown hazard on the seafloor. These results show that Arctic environments are areas of active seafloor processes that can have consequences on future marine infrastructure. Understanding the triggers of marine geohazards, in combination with standard regional assessments performed by the Geological Survey of Canada, will allow stakeholders and decision-makers to properly manage seabed infrastructure in a changing and active marine environment.
Summary(Plain Language Summary, not published)
Our results show that Arctic environments are areas of active seafloor processes that can have consequences on future seafloor infrastructures. Understanding the triggers of marine geohazards, in combination with standard regional assessments performed by the Geological Survey of Canada, will allow stakeholders and planners to properly manage seabed infrastructure in a changing and active marine environment.
GEOSCAN ID327915

 
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