A contoured (interval 20m) general reference map of the island showing settlement, mining areas, railways, roads and tracks of Norfolk Islands.

Legacy product - no abstract available

In June 1980 the Department of Housing and Construction (DHC) completed a report on the proposed water supply iand swerage project for Norfolk Island (Goldfinch & Cross, 1980). This report requested that the Bureau of Mineral Resources (BMR) implement the following recommendations: 1. Undertake hydrogeological investigations on Norfolk Island as recommended in a Groundwater reprot on Norfolk Island (Abell, 1976). 2. Undertake investigations, drilling and testing as appropriate to provide observation and production bores in either or both of the Broken Bridge/Mission Creek valleys. A sufficient number of bores are to be drilled so that a production rate of not less than 10.4 L/sec is achieved with at least one bore in exess of minimum requirements to provide standby capacity. Each production bore is to be cased and fitted with screens. The main objective of the survey was a hydrogeological/geophysical investigation in the Broken Bridge - Mission Creek valleys leading to the selection of drill sites and recommendations on drilling to ascertain whether a groundwater supply at deeper levels on the island can be developed free of pollution from human or other agencies.

This is a post-cruise report for the collaborative Australia/France searfloor mapping survey east of Norfolk Island. Regional settings, survey design and preliminary results are discussed.

Norfolk Island in the southwest Pacific Ocean has an area of 35 k m2 and rises to an altitude of just over 300 m. It is an erosional remnant of a volcanic complex consisting of subaerial basaltic lava flows and pyroclastics built on a submarine pile of hyaloclastite deposits and pillow lavas. A deep weathering profile has developed in the volcanic succession since eruptive activity ceased during the late Pliocene 2.3 Ma ago. Throughout the island there is an upper water table aquifer in porous alluvium and weathered basaltic rock. At the base of the weathered profile groundwater moves towards sea level through a complex network of fractures and other interconnected openings in volcanic bedrock. Semi-confined aquifers occur in fractured basalt flows and interbedded basaltic pyroclastics (tuffs and agglomerates). However, the extent and quality of deep groundwater below sea level needs more evaluation. The groundwater storage on Norfolk Island is tapped by more than 450 wells and bores.

Legacy product - no abstract available

This map shows the boundaries of the Maritime Security Zones for each port for the purpose of the Maritime Transport & Office Security Act 2003. 1 Sheet (Colour) May 2010 Not for sale or public distribution Contact Manager LOSAMBA project, PMD

This map shows the boundary of the security regulated port for the purpose of the Maritime Transport & Office Security Act 2003. 1 Sheet (Colour) April 2010 Not for sale or public distribution Contact Manager LOSAMBA project, PMD

At 1:15,000 scale, this map is larger than previous editions. It is printed on both sides, with the reverse portraying colourful photographs and text describing Norfolk Islands flora and fauna, history, things to do and see etc. This map is sold as a flat or folded product through Geoscience Australia`s Sales Centre or our map retailers, located throughout Australia.

This map has been created to update the old Crimes at Sea maps produced in 2000. These maps have been checked & approved by the Attorney Generals Office April 2013. There are 13 maps in the series plus the main map showing all of the Australian Territory. The AAT maps have not been released to the public as yet. Located in M:\Products\Australias Crimes Act Offshore Areas\products