Submarine Mass Failure Cores from Frobisher Bay (Nunavut) aboard CCGS Amundsen
This data is currently in relation to twelve piston cores collected aboard CCGS Amundsen, one on cruise 2014805, two on cruise 2015805, six on cruise 2016804, and three on cruise 2017805. Information about these cores (Location, length, grain size, radiocarbon dates, etc.) can be found by searching the NRCan Expedition Database.
Simple
- Date (Publication)
- 2018-11-02
- Other citation details
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Bell, T., Forbes, D. and Deering, R. (2018) Submarine Mass Failure Cores from Frobisher Bay (Nunavut) aboard CCGS Amundsen. Waterloo, Canada: Canadian Cryospheric Information Network (CCIN). Unpublished Data
- Purpose
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These cores were collected to both date submarine mass failure events and to better understand the stratigraphic context in which they occurred. This information will be part of a larger project on submarine mass failures, trying to better understand their seabed contexts and triggering mechanisms in Baffin Island fjords.
- Status
- Completed
Canadian Cryospheric Information Network
-Polar Data Catalogue
200 University Avenue West, University of Waterloo
,Waterloo
,Ontario
,N2L 3G1
,Canada
polardata.ca
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Polar Data Catalogue Thesaurus (Canada)
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Baffin Island
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Frobisher Bay
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Geomorphology
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Marine sediments
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Mass movements
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Seabed
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Sediment cores
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Stratigraphy
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- Place
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Frobisher Bay, Baffin Island, Nunavut, Canada
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- Access constraints
- Other restrictions
- Use constraints
- Other restrictions
- Other constraints
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Terms of Use of the Polar Data Catalogue: https://www.polardata.ca/pdcinput/public/termsofuse
- Metadata language
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eng; CAN
- Topic category
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- Environment
- Begin date
- 2014-10-04
- End date
- 2017-07-14
- Supplemental Information
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Summary: Submarine mass failures are potentially destructive movements of sediment on the seabed. These events are capable of destroying seabed infrastructure and generating tsunami waves which could inundate coastal communities. They also leave a distinct scar on the seabed that can be seen using sonar. To better understand these events, sediment cores are taken from these scars. These sediment records can be used to examine the sediments underlying the failure as well as date when the failure occurred. Using cores from multiple events a timeline of events and potential triggering mechanisms can be inferred. Research Program(s): ArcticNet. For further information: tbell@mun.ca tbell@mun.ca
- Distribution format
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Digital file
(1.0
)
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Canadian Cryospheric Information Network
-Polar Data Catalogue
200 University Avenue West, University of Waterloo
,Waterloo
,Ontario
,N2L 3G1
,Canada
- Included with dataset
- No
- File identifier
- 5851195d-e72f-4ffd-a81a-9cf8068efbcb XML
- Metadata language
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eng; CAN
- Character set
- UTF8
- Hierarchy level
- Dataset
- Date stamp
- 2022-04-08T12:59:41
- Metadata standard name
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North American Profile of ISO 19115:2003
- Metadata standard version
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2009-01-01
Canadian Cryospheric Information Network
-Polar Data Catalogue
200 University Avenue West, University of Waterloo
,Waterloo
,Ontario
,N2L 3G1
,Canada
Overviews
Spatial extent
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ARICE Metadata Catalogue