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The Marshall Islands consist of two archipelagic island chains of 30 atolls and 1,152 islands, which form two parallel groups—the "Ratak" (sunrise) chain and the "Ralik" (sunset) chain. The Marshalls are located in the North Pacific Ocean and share maritime boundaries with Micronesia and Kiribati .
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.
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]
Located between Hawaii and Australia, the country is one of the world’s youngest and smallest, but not many people will ever experience the warmth of the Marshall Islands – both its tropical ...
Johnston Atoll is located between the Marshall Islands and the Hawaiian Islands. Johnston Island has been significantly increased in size through coral dredging. Johnston Atoll is a 1,300-hectare (3,200-acre) atoll in the North Pacific Ocean , located about 750 nautical miles (1,390 km ; 860 mi ) southwest of the island of Hawaiʻi , and is ...
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).
Map showing the location of Midway Atoll in the Hawaiian island chain. Midway Atoll (colloquial: Midway Islands; Hawaiian: Kuaihelani, lit. 'the backbone of heaven'; Pihemanu, 'the loud din of birds') [3] [4] is a 2.4 sq mi (6.2 km 2) atoll in the North Pacific Ocean.
The Marshallese recognized four main ocean swells: the rilib, kaelib, bungdockerik and bundockeing. [2] Navigators focused on effects of islands in blocking swells and generating counterswells to some degree, but they mainly concentrated on refraction of swells as they came in contact with undersea slopes of islands and the bending of swells around islands as they interacted with swells coming ...