<div>The Abbot Point to Hydrographers Passage bathymetry survey was acquired for the Australian Hydrographic Office (AHO) onboard the RV Escape during the period 6 Oct 2020 – 16 Mar 2021. This was a contracted survey conducted for the Australian Hydrographic Office by iXblue Pty Ltd as part of the Hydroscheme Industry Partnership Program. The survey area encompases a section of Two-Way Route from Abbot Point through Hydrographers Passage QLD. Bathymetry data was acquired using a Kongsberg EM 2040, and processed using QPS QINSy. The dataset was then exported as a 30m resolution, 32 bit floating point GeoTIFF grid of the survey area.</div><div>This dataset is not to be used for navigational purposes.</div>

The Australian Geological Survey Organistaion (AGSO) has produced a set of digital bathymetry, gravity and magnetic grids for the southwest quadrant of Australia (24 - 46S, 106-140E), using all available land, marine and satellite data. The work was done in cooperation with Desmond Fitzgerald & Associates (DFA), and with significant bathymetric data input from the Australian Hydrographic Office (AHO). The results were obtained by performing a network adjustment on marine ship-track data, and combining these with onshore and satellite-derived data.

Legacy product - no abstract available

Flythrough of the Austrlalian Margin (not including the northern margin) showing detail of the Exmouth Plateau, Perth Canyon, Murray Canyons, NSW Slope and Great Barrier Reef. Gridded bathymetry data shown in this product was sourced from GA and James Cook University.

This flythrough was produced on CD for a media launch held on 17/11/05 in Cairns.

The definition of Australia?s marine jurisdiction, under the 1982 United Nations Convention on the Law of the Sea (LOS), may need to take into account the location of the 2500m seafloor contour. A large amount of water depth data from a variety of sources have been used to produce bathymetric grids and contours around the Australian region by the LOS Study Group at Geoscience Australia. It is well known that the data are far from perfect, containing problems in depth soundings as well as navigation. The LOS Group wished to determine a quantitative measure for the accuracy of the data they have used. This study took the data used in the Naturaliste Plateau area and determined the intersection points of all the survey tracks. From this it computed interpolated water depths at the intersections and calculated mistie values between the intersecting surveys. In all 12411 intersections were found. Not all were useable, mainly due to the long intervals between soundings. Some surveys contained numerous intersections in very shallow water (~ 40 m) with excellent mistie statistics (+/- 1 m), but it was felt that these could unfairly bias the derived statistics. Taking these considerations into account reduced the number of intersecting points and mistie values that went into the statistical analysis to 5606. The procedures and programs employed in this report can easily be extended to all the other areas investigated by the LOS Group. This will be done in due course, with a future report summarising the statistics for each of the LOS study areas and making recommendations for the improvement of the bathymetric data held by Geoscience Australia.

Please note: This product has been superseded by 50m Multibeam Dataset of Australia 2018. - This tile contains all multibeam data held by Geoscience Australia on August 2012 within the specified area. The data has been gridded to 50m resolution. Some deeper data has also been interpolated within the mapped area. The image provided can be viewed on the free software CARIS Easyview, available from the CARIS website: www.caris.com under Free Downloads.

Please note: This product has been superseded by 50m Multibeam Dataset of Australia 2018. - This tile contains all multibeam data held by Geoscience Australia on August 2012 within the specified area. The data has been gridded to 50m resolution. Some deeper data has also been interpolated within the mapped area. The image provided can be viewed on the free software CARIS Easyview, available from the CARIS website: www.caris.com under Free Downloads.

Surveying of nearshore areas in the Vestfold Hills using high resolution multibeam swath bathymetry provides both a detailed digital bathymetric model and information on sediment acoustic backscatter. Combined with underwater video transects and sediment sampling, these data can be used to identify and map geomorphic units. Six geomorphic units identified in the survey region include: Rocky outcrops, sediment-floored basins, pediments, steep-sided valleys, scarps and sheltered embayments. In addition to geomorphic units, the data reveal sedimentary structures that provide insights into sediment transport and erosion in the area. Ice keel pits and scours are common while seafloor channels, scour depressions and sand ribbons indicate transport and deposition by wind-driven currents and oceanographic circulation. Gullies and sediment lobes on steep slopes indicate mass movement of sediment. The sheltered embayments preserve a mantle of boulder sand probably deposited by cold-based glaciers. Automated techniques utilizing the bathymetric grid and backscatter to map landforms are useful in defining reproducible boundaries between geomorphic units but cannot easily be adapted to accurately classify the variations in sea floor texture and structure imaged by these data.

Please note: This product has been superseded by 50m Multibeam Dataset of Australia 2018. - This tile contains all multibeam data held by Geoscience Australia on August 2012 within the specified area. The data has been gridded to 50m resolution. Some deeper data has also been interpolated within the mapped area. The image provided can be viewed on the free software CARIS Easyview, available from the CARIS website: www.caris.com under Free Downloads.