Submarine geomorphology of the northeastern Baffin Island fiords and cross-shelf troughs

This paper presents a series of 50 geomorphological maps of the seabed of northeastern Baffin Island fiords and cross-shelf troughs, in eastern Arctic Canada. The mapping was produced using swath bathymetry imagery from multiple bathymetry datasets. A total of 24 types of landform were systematicall...

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Bibliographic Details
Main Authors: Etienne Brouard (7214678), Patrick Lajeunesse (7214681)
Format: Dataset
Language:unknown
Published: 2019
Subjects:
Online Access:https://doi.org/10.6084/m9.figshare.9569684.v3
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record_format openpolar
spelling ftsmithonian:oai:figshare.com:article/9569684 2023-05-15T14:50:55+02:00 Submarine geomorphology of the northeastern Baffin Island fiords and cross-shelf troughs Etienne Brouard (7214678) Patrick Lajeunesse (7214681) 2019-08-13T06:22:16Z https://doi.org/10.6084/m9.figshare.9569684.v3 unknown https://figshare.com/articles/dataset/Submarine_geomorphology_of_the_northeastern_Baffin_Island_fiords_and_cross-shelf_troughs/9569684 doi:10.6084/m9.figshare.9569684.v3 CC BY 4.0 CC-BY Ecology Inorganic Chemistry Environmental Sciences not elsewhere classified Biological Sciences not elsewhere classified Geomorphology submarine landforms bathymetry glacial geomorphology Arctic Canada fjords glacial troughs Dataset 2019 ftsmithonian https://doi.org/10.6084/m9.figshare.9569684.v3 2021-12-20T01:14:36Z This paper presents a series of 50 geomorphological maps of the seabed of northeastern Baffin Island fiords and cross-shelf troughs, in eastern Arctic Canada. The mapping was produced using swath bathymetry imagery from multiple bathymetry datasets. A total of 24 types of landform were systematically mapped (>55,000 landforms) and reflect processes linked to subglacial, ice-marginal or paraglacial to postglacial environments. The landforms record the transition of the seabed from being covered by a marine-terminating ice sheet to the establishment of postglacial conditions. The landform assemblages allow the distinction of ice-flows orientation and ice-stream pathways along fiords and cross-shelf troughs. The multiple moraines and grounding-zone wedges indicate that the ice margin stabilized during retreat and that the overall deglaciation occurred by steps. These maps provide a framework for future investigations in northeastern Baffin Island fiords and shelf and can also provide a template for future seabed geomorphological studies in Arctic Canada. Dataset Arctic Baffin Island Baffin Ice Sheet Unknown Arctic Baffin Island Canada
institution Open Polar
collection Unknown
op_collection_id ftsmithonian
language unknown
topic Ecology
Inorganic Chemistry
Environmental Sciences not elsewhere classified
Biological Sciences not elsewhere classified
Geomorphology
submarine landforms
bathymetry
glacial geomorphology
Arctic Canada
fjords
glacial troughs
spellingShingle Ecology
Inorganic Chemistry
Environmental Sciences not elsewhere classified
Biological Sciences not elsewhere classified
Geomorphology
submarine landforms
bathymetry
glacial geomorphology
Arctic Canada
fjords
glacial troughs
Etienne Brouard (7214678)
Patrick Lajeunesse (7214681)
Submarine geomorphology of the northeastern Baffin Island fiords and cross-shelf troughs
topic_facet Ecology
Inorganic Chemistry
Environmental Sciences not elsewhere classified
Biological Sciences not elsewhere classified
Geomorphology
submarine landforms
bathymetry
glacial geomorphology
Arctic Canada
fjords
glacial troughs
description This paper presents a series of 50 geomorphological maps of the seabed of northeastern Baffin Island fiords and cross-shelf troughs, in eastern Arctic Canada. The mapping was produced using swath bathymetry imagery from multiple bathymetry datasets. A total of 24 types of landform were systematically mapped (>55,000 landforms) and reflect processes linked to subglacial, ice-marginal or paraglacial to postglacial environments. The landforms record the transition of the seabed from being covered by a marine-terminating ice sheet to the establishment of postglacial conditions. The landform assemblages allow the distinction of ice-flows orientation and ice-stream pathways along fiords and cross-shelf troughs. The multiple moraines and grounding-zone wedges indicate that the ice margin stabilized during retreat and that the overall deglaciation occurred by steps. These maps provide a framework for future investigations in northeastern Baffin Island fiords and shelf and can also provide a template for future seabed geomorphological studies in Arctic Canada.
format Dataset
author Etienne Brouard (7214678)
Patrick Lajeunesse (7214681)
author_facet Etienne Brouard (7214678)
Patrick Lajeunesse (7214681)
author_sort Etienne Brouard (7214678)
title Submarine geomorphology of the northeastern Baffin Island fiords and cross-shelf troughs
title_short Submarine geomorphology of the northeastern Baffin Island fiords and cross-shelf troughs
title_full Submarine geomorphology of the northeastern Baffin Island fiords and cross-shelf troughs
title_fullStr Submarine geomorphology of the northeastern Baffin Island fiords and cross-shelf troughs
title_full_unstemmed Submarine geomorphology of the northeastern Baffin Island fiords and cross-shelf troughs
title_sort submarine geomorphology of the northeastern baffin island fiords and cross-shelf troughs
publishDate 2019
url https://doi.org/10.6084/m9.figshare.9569684.v3
geographic Arctic
Baffin Island
Canada
geographic_facet Arctic
Baffin Island
Canada
genre Arctic
Baffin Island
Baffin
Ice Sheet
genre_facet Arctic
Baffin Island
Baffin
Ice Sheet
op_relation https://figshare.com/articles/dataset/Submarine_geomorphology_of_the_northeastern_Baffin_Island_fiords_and_cross-shelf_troughs/9569684
doi:10.6084/m9.figshare.9569684.v3
op_rights CC BY 4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.6084/m9.figshare.9569684.v3
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