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The sea around Pacific islands has risen 7mm a year since 1993, which is more than twice the rate of the worldwide average. In Kwajalein , there is a high risk of permanent flooding; when sea level rise to 1 meter, 37% of buildings will be permanently flooded in that scenario.
The Marshall Islands (Marshallese: Ṃajeḷ), [5] officially the Republic of the Marshall Islands (Marshallese: Aolepān Aorōkin Ṃajeḷ), [note 1] is an island country west of the International Date Line and north of the equator in the Micronesia region of the Northwestern Pacific Ocean.
Ebon Atoll (Marshallese: Epoon, [ɛbʲɔːnʲ] [1]) is a coral atoll of 22 islands in the Pacific Ocean, forming a legislative district of the Ralik Chain of the Marshall Islands. Its land area is 5.75 square kilometers (2.22 sq mi), and it encloses a deep lagoon with an area of 104 square kilometers (40 sq mi).
Map from National Atlas of the United States. Kwajalein is the 14th largest coral atoll as measured by area of enclosed water. Comprising 97 islands and islets, it has a land area of 16.4 km 2 (6.3 sq mi) and surrounds one of the largest lagoons in the world, with an area of 2,174 km 2 (839 sq mi).
The following outline is provided as an overview of and topical guide to the Marshall Islands: Marshall Islands – sovereign Micronesian island nation located in the western North Pacific Ocean, north of Nauru and Kiribati, east of the Federated States of Micronesia, and south of the U.S. territory of Wake Island, to which it lays claim. [1]
Namu Atoll (Marshallese: Naṃo, [1]) is a coral atoll of 54 islands in the Pacific Ocean, and forms a legislative district of the Ralik Chain of the Marshall Islands.Its total land area is only 6.27 square kilometers (2.42 sq mi), but that encloses a lagoon of 397 square kilometers (153 sq mi).
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Island locations were represented by shells tied to the framework, or by the lashed junction of two or more sticks. The threads represented prevailing ocean surface wave-crests and directions they took as they approached islands and met other similar wave-crests formed by the ebb and flow of breakers. Individual charts varied so much in form ...