Seismic refraction results over the D'entrecasteaux zone west of the New Hebrides arc
Geoscience and resource information for Tuvalu, a bibliography, 19 March 1985
Wave energy utilization mission, 5 - 21 November 1984
Assessment of the potential of the North Malaita alluvial garnets for a cottage industry producing tumble-polished stones, 9 - 18 June, 1984
Trip report to Vanuatu - Solomon Islands, 16-22 October 1994
A report on research vessel activity in Fiji's Exclusive Economic Zone in 1991 and 1992
Petroleum source rock survey in the Solomon Islands and Vanuatu, Southwest Pacific
Sanitation and wastewater management in Tonga
SIDS DOCK Pacific Regional Meeting Outcomes
Site-specific earthquake hazard determinations in capital cities in the South Pacific
Taveuni volcanic hazards workshops, National Level - Suva, 21-23 June 1999, Island Level - Waiyevo, Taveuni, 13-14 December 1999
Economic impact of natural disasters on development in the Pacific; volume 1: research report, May 2005
Economic impact of natural disasters on development in the Pacific, volume 2: economic assessment tools, May 2005
A high-resolution bathymetric mapping survey was conducted for the seabed surrounding the island of Efate in Vanuatu.The bathymetry chart contained here is the second part of the overall bathymetry chart produced for Efate Island in Vanuatu. This bathymetric map is a blend of multibeam (MBES), and singlebeam (SBES) echosounder data. All slope angles exceeding 60 degrees (degrees from horizontal) were interpreted as scarps. Any Inclined area of the seafloor that was laterally confined by distinctive slopes, with or without an upslope headscarp, was interpreted as a channel.
This record holds the Technical report describing a SOPAC Division marine survey carried out for Kiribati, on the islands of Abaiang, Tarawa, Abemama, Banaba and Onotoa.
This report describes the high-resolution bathymetric mapping survey of the seabed surrounding the islands of Abaiang, Tarawa, Abemama, Banaba and Onotoa in Kiribati.
The work was initiated by the Pacific Islands Applied Geoscience Commission (SOPAC) and the European Union (EU) Reducing Vulnerability of Pacific ACP States
This record holds the PDF format of the bathymetry chart of Forari Bay in Efate, Vanuatu. The chart shows the 3-dimensional bathymetry map of Forari Bay showing shallow to deep from red to blue. Two times vertical exaggeration. Chart is the result of high-resolution bathymetric mapping survey of the seabed surrounding Forari Bay in Vanuatu using a blend of multibeam (MBES), and singlebeam (SBES) echosounder data.
This record holds the Bathymetry chart of Mele Bay showing shallow to deep, from red to blue. Two times vertical exaggeration. Chart is the result of the high-resolution bathymetric mapping survey of the seabed surrounding Mele Bay, South West Efate Island in Vanuatu. This bathymetric map is the blend of multibeam (MBES), and singlebeam (SBES) echosounder data. This work was initiated by the SOPAC/EU Reducing Vulnerability of Pacific ACP States Project.
A high-resolution bathymetric mapping survey of the seabed surrounding the island of Efate in Vanuatu.This bathymetric map is a blend of multibeam (MBES), and singlebeam (SBES) echosounder data. All slope angles exceeding 60 degrees (degrees from horizontal) were interpreted as scarps. Any Inclined area of the seafloor that was laterally confined by distinctive slopes, with or without an upslope headscarp, was interpreted as a channel.
A high-resolution bathymetric mapping survey of the seabed surrounding the island of Efate in Vanuatu.This bathymetric map is a blend of multibeam (MBES), and singlebeam (SBES) echosounder data. All slope angles exceeding 60 degrees (degrees from horizontal) were interpreted as scarps. Any Inclined area of the seafloor that was laterally confined by distinctive slopes, with or without an upslope headscarp, was interpreted as a channel.
A high-resolution bathymetric mapping survey of the seabed surrounding the island of Efate in Vanuatu.This bathymetric map is a blend of multibeam (MBES), and singlebeam (SBES) echosounder data. All slope angles exceeding 60 degrees (degrees from horizontal) were interpreted as scarps. Any Inclined area of the seafloor that was laterally confined by distinctive slopes, with or without an upslope headscarp, was interpreted as a channel.