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.
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.
This record holds the Bathymetry chart of Havannah Bay showing shallow to deep, from red to blue, with two times vertical exaggeration. Chart is the result of the high-resolution bathymetric mapping survey of the seabed surrounding Port Havannah Harbour in Vanuatu. This bathymetric map is a 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.
This report describes a high-resolution bathymetric mapping survey of the seabed surrounding the island of Efate in Vanuatu, by the Pacific Islands Applied Geoscience Commission
(SOPAC). The survey was carried out over a period of 25
days in August 2003, resulting in the acquisition of over 600 line kilometres of MBES data.
The resultant compilation was used to produce
bathymetry charts of Efate at scales of 1 : 100 000 and 1 : 50 000, with more detailed charts of
Mele Bay, Forari Bay and Havannah Bay at 1 : 20 000.
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.