The Code of the Federated States of Micronesia (FSM) was amended to include the Exclusive Economic Zone (EEZ), to increase the size of its Territorial Sea and to be inclusive of the current political status of FSM and other purpose as it deem fit (16 December 1988)
The Marine Zones (Declaration) Act 2011 repeals the Marine Zones (Declaration) Act 1983. It states that the exclusive economic zone comprises those waters beyond the territorial sea of Kiribati, but within a distance of two hundred (200) nautical miles from the baseline of Kiribati, shall be the exclusive economic zone of the Republic of Kiribati.
The Marine Zones (Declaration) Act 2011 repeals the Marine Zones (Declaration) Act 1983. It states that the "Contiguous Zone" means waters beyond the territorial sea within a distance of twenty-four (24) nautical miles from the baselines from which the breadth of the territorial sea is measured.
The Marine Zones (Declaration) Act 2011 repeals the Marine Zones (Declaration) Act 1983. It states that the exclusive economic zone comprises those waters beyond the territorial sea of Kiribati, but within a distance of two hundred (200) nautical miles from the baseline of Kiribati, shall be the exclusive economic zone of the Republic of Kiribati.
The Marine Zones (Declaration) Act 2011 repeals the Marine Zones (Declaration) Act 1983. It states that the exclusive economic zone comprises those waters beyond the territorial sea of Kiribati, but within a distance of two hundred (200) nautical miles from the baseline of Kiribati, shall be the exclusive economic zone of the Republic of Kiribati.
Based on section 102 and 103 of the Act that amends the Code of the Federated States of Micronesia, it describes the territorial sea as being established by twelve nautical miles' breadth. The inner boundary of the Territorial Sea of each island or atoll is the baseline. The outer boundary is a line, every point of which is twelve nautical miles seaward of the nearest point of the baseline.
This layer shows the 12M maritime zone for the Republic of Marshall Islands which is highlighted in the Marshall Islands Maritime Zone Act 2016.
In Part 3 of the The Maritime Zones Act 2013 states that the exclusive economic zone of Niue comprises those areas of the sea,
seabed and subsoil that are beyond and adjacent to the territorial sea having as their outer limits a line measured seaward from the baseline described in section 4, every point of which line is not more than 200 nautical miles from the nearest point of the baseline.
https://www.un.org/depts/los/LEGISLATIONANDTREATIES/PDFFILES/niu_mariti…
The Regional Seas programme of UNEP commenced in 1974 and since that time
considerable advances have been made in the development of regional action plans and
conventions for the protection of the marine and coastal areas of some eleven regions world-
wide. Following these developments UNEP has encouraged inter-regional co-operation in
addressing various issues of environmental concern through the organisation of international
meetings and inter-regional symposia. This volume contains the record of one such symposium,
The tropical seas are liberally sprinkled with coral islands.
Many of them are associated with continents and large continental islands, in relatively shallow water, rising from continental shelves. Many, also, are in deep water - atolls, barrier reef islets round high islands, almost atolls', tops of drowned karsts, and a few moderately elevated atolls. These last are among the most fascinating of all, scientifically.
An article taken from the Atoll Research Bulletin No.272|Kept at Greg's collection|Available online
Call Number: VF 1564 [EL}
Pesticides as covered in the project include acaricides,
biological pesticides (bacteria, viruses), defoliants,
dessicants, fumigants, fungicides, herbicides, insecticides,
molluscicides, nematicides, rodenticides and synergists.
Pesticides included are those used in plant protection, in
animal health (products for external use only), in human
health programmes and for urban pest control.
The main topographical features of Samoa are rugged mountains of volcanic origin, surrounded by flat and rolling coastal plains. All the islands of Samoa were formed by volcanic activity. Savai'i is regarded as still volcanically active with its most recent eruption producing lava flows between 1905 and 1911. A large percentage of Samoan soils are porous, shallow and clay in texture.
Also available online|A PICCAP-GEF funded project
Call Number: 551.6 UNI [EL],302.2 GOV,VF 2682,INT-CON
Physical Description: xi, 50 p. ; 29 cm
There is a high level of uncertainty with the specific estimation of pollutant loads. A large body of work has
been completed that provided qualitative and quantitative data; however, the noting of data gaps and inherent uncertainties of the methods used have qualified much of the quantitative data. Much of the data are based on rapid assessment methods that utilise generic loading rates, assumed waste flow composition, typical production methods, local production rates. Unfortunately, production rate data are inconsistently available and are difficult to verify.