Scientific article - Pacific Science 2008 (62 : 4) 495-498.
Scientific article - Bulletin BOC 2008 128(4)
Scientific article: Pacific Science 2008 (62 : 4 ) 499-507
Photocopy of an article published in Geo 9 (2): 70-77
Scientific publication: Micronesica 39 (2): 171-295 (2007)
A report published by the Atoll Research Programme, University of the South Pacific 1997 for
Nauru Departments of: Island Development and Industry, Education and Health and Nauru Fisheries and Marine Resources of the Government of the Republic of NAURU
with financial support from UNESCO
via UNESCO Office for the Pacific States, W. Samoa.
Scientific article published in the Pacific Science (2008) vol. 62, no. 4: 499-507
pdf 1 pager. graph downloaded from BOM 2021
Legislation
4-page summary from the United Nations Framework Convention on Climate Change
Graph from OurWorldInData
Report presented to the Fourth Pacific Meteorological Council Meeting held in Honiara from 14-18 August, 2017.
Report - 9 pages
Report - 49 pages. Porduced with support from the European Union and the German Government (GIZ).
The [Allen Coral Atlas](https://allencoralatlas.org/) combines high resolution satellite imagery, machine learning and field data to produce globally consistent benthic and geomorphic maps of the world's coral reefs. The Atlas is funded primarily by [Vulcan Inc.](https://www.vulcan.com) (founded by the late Paul G.
Map of the Nauru island landcover, with country-level summary of the different landcover classes and designation.
Map of the Nauru Island landuse, with country-level summary of the different landuse classes and designation.
Nauru, in the central Pacific Ocean, is a raised atoll capping a volcanic seamount arising from an ocean floor depth of 4300m. The land area is 22km, and the island rises to 70m above sea level. Drilling has proved dolomitised limestone of upper Miocene or younger age to a depth of 55m below sea level. Gravity and magnetic surveys indicate that the limestone probably overlies volcanic bedrock at a depth of about 500m. Reverse-circulation drilling and geoelectrical probes indicate that there is a discontinuous freshwater layer averaging 5m thick beneath Nauru.
The problem of seawater intrusion in coastal aquifers and oceanic islands is not a new one and a great deal of research has been undertaken since the late 19th century. The first model was developed in 1888 and is known as the Ghyben-Herzberg. It is a simple model based on the hydrostatic balance between fresh and saline water. With the advent of large computing capacity over the past few decades, more sophisticated models have been developed for the simulation of seawater intrusion and upconing of saline water beneath a pumping well.