A seabeam and sampling survey of newly discovered Tavui caldera near Rabaul, Papua New Guinea, 7-9 May 1990
Initial report of 1986 R.V.Moana wave cruise MW-86-02 in the Kiribati/Tuvalu region, Central Pacific Ocean, Pohnpei to Honolulu, 21 February to 15 March 1986
Mineral resource studies in the Southwest Pacific, 1982
SPOT 1 image utilization, assessment, results
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
Reducing the impacts of environmental emergencies through early warning and preparedness, the case of El Nino Southern Osillation (ENSO), -the Fiji case study-
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
The Costs And Benefits Of Introducing Standards And Labels For Electrical Appliances In PICs
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.