Kerguelen-Heard Island region - Mapping Under Sea Geomorphology

The geomorphology was digitised using contours derived from the DEM created by Dr. R. Beaman from James Cook University for Geoscience Australia. The data, the metadata record and the report related to the creation of that DEM are available on the Geoscience Australia website: Name of data set: Kerg...

Full description

Bibliographic Details
Other Authors: BROLSMA, HENK (hasPrincipalInvestigator), BROLSMA, HENK (processor), Australian Antarctic Data Centre (publisher)
Format: Dataset
Language:unknown
Published: Australian Antarctic Data Centre
Subjects:
geoscientificInformation
oceans
planningCadastre
GEOMORPHIC LANDFORMS/PROCESSES
EARTH SCIENCE
SOLID EARTH
BATHYMETRY/SEAFLOOR TOPOGRAPHY
BATHYMETRY
Geomorphology
Mapping
ECHO SOUNDERS
MBES &gt
Multibeam Mapping System
SATELLITES
SHIPS
OCEAN &gt
SOUTHERN OCEAN &gt
HEARD AND MCDONALD ISLANDS
INDIAN OCEAN &gt
KERGUELEN ISLANDS
SOUTHERN OCEAN
GEOGRAPHIC REGION &gt
POLAR
Southern Ocean
Kerguelen
Heard Island
Kerguelen Islands
Indian
Heard
McDonald Islands
Online Access:https://researchdata.ands.org.au/kerguelen-heard-island-sea-geomorphology/701203
https://doi.org/10.26179/5b9b5078b6610
https://data.aad.gov.au/metadata/records/Kerg_Heard_Plateau_Under_Sea_Geomorphology
http://nla.gov.au/nla.party-617536
Description
Summary:The geomorphology was digitised using contours derived from the DEM created by Dr. R. Beaman from James Cook University for Geoscience Australia. The data, the metadata record and the report related to the creation of that DEM are available on the Geoscience Australia website: Name of data set: Kerguelen Plateau Bathymetric Grid 2010 Catalogue number: 71552 https://ecat.ga.gov.au/geonetwork/srv/eng/catalog.search?node=srv#/metadata/a05f7893-007f-7506-e044-00144fdd4fa6 Digitising: It must be stressed that neither seismic data, sea floor sediments, nor sea floor biota were used to determine the sea floor geomorphology. The description on how the geomorphology was derived is described in the attached report. The features described as slopes from the 900m to 1300m isobaths and from the 1300m to 2500m isobaths were identified for fisheries purposes and not geomorphology purposes. A geomorphologist may combine these slopes into a single feature. Some of the larger shallow features identified as banks may more properly be identified as plateaus. It would require a more in depth analysis of the DEM, slopes and sediments to accurately identify the feature as a bank or plateau.

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