Geography of the Marshall Islands

Home | Category: Nature, Environment, Animals

GEOGRAPHY OF THE MARSHALL ISLANDS

The Marshall Islands are located in Oceania, consists of 29 atolls and five isolated islands in the North Pacific Ocean, about halfway between Hawaii and Australia; the atolls and islands are situated in two, almost-parallel island chains: the Ratak (Sunrise) group and the Ralik (Sunset) group; the total number of islands and islets is about 1,225; 22 of the atolls and four of the islands are uninhabited. Its geographic coordinates are 9 00 N, 168 00 E. [Source: CIA World Factbook, 2023]

Area: total: 181 square kilometers; land: 181 square kilometers; water: 0 square kilometers. note: the archipelago includes 11,673 square kilometers of lagoon waters and encompasses the atolls of Bikini, Enewetak, Kwajalein, Majuro, Rongelap, and Utirik; ranking compared to other countries in the world: 216. It is about about the size of Washington, DC. [Source: CIA World Factbook 2023]

The islands of Bikini and Enewetak are former US nuclear test sites; Kwajalein atoll, famous as a World War II battleground, surrounds the world's largest lagoon and is used as a US missile test range; the island city of Ebeye is the second largest settlement in the Marshall Islands, after the capital of Majuro, and one of the most densely populated locations in the Pacific Land Boundaries: total: 0 kilometers; Coastline: 370.4 kilometers; Maritime claims: territorial sea: 12 nautical miles; contiguous zone: 24 nautical miles; exclusive economic zone: 200 nautical miles.

Topography: low coral limestone and sand islands. Elevation: highest point: East-central Airik Island, Maloelap Atoll 14 meters; lowest point: Pacific Ocean 0 meters; mean elevation: 2 meters.

Land Use: agricultural land: 50.7 percent (2018 estimate). Arable Land: 7.8 percent (2018 estimate); permanent crops: 31.2 percent (2018 estimate); permanent pasture: 11.7 percent (2018 estimate); forest: 49.3 percent (2018 estimate); other: 0 percent (2018 estimate). Irrigated Land: 0 square kilometers (2022). [Source: CIA World Factbook 2023]

Population Distribution: most people live in urban clusters found on many of the country's islands; more than two-thirds of the population lives on the atolls of Majuro and Ebeye.

Climate: tropical; hot and humid; wet season May to November; islands border typhoon belt. Natural Hazards: infrequent typhoons

Micronesia, Marshall Islands, Palau, Marianas and Caroline Islands

The region known as Micronesia ("small islands") is divided geographically into three archipelagoes: the Marshall Islands, the Marianas (including Guam and Saipan) and the Caroline Islands. The four states of the Federated States of Micronesia—Kosrae, Pohnpei, Chuuk and Yap— are all part of the Caroline Islands, which in turn are divided into the Western Caroline Islands (Palau, Yap and Chuck) and the Eastern Caroline Islands (Pohnpei and Kosrae).

Each group of islands has a "district center," with an international airport, and the majority of the government offices, medical facilities and tourist facilities. The main district centers are Majuro (Marshall Islands), Koror (Palau), Saipan (Northern Marianas), Pohnpei, Weno Island (Chuuk), Yap Proper (Yap) and Kosrae.

The Federated States of Micronesia (FSM) is the name of a new country created in 1979 from former Japanese Pacific territories taken over by the U.S. after World War II. It includes the island states of Yap, Chuuk, Pohnpei, Kosrae, and numerous atolls in the area of these island states. The term Micronesia is also used to describe the islands in a region that stretch from Hawaii to the Philippines and also includes Guam, the Commonwealth of the Northern Marianas, the Republic of Palau and the Republic of the Marshall Islands.

The islands of the region of Micronesia are scattered across an area larger than the United States, but the total land area of the Federated States of Micronesia (FSM), Guam, the Commonwealth of the Northern Marianas, the Republic of Palau and the Republic of the Marshall Islands is two thirds that of Rhode Island. In 1965, 96 of the 2,100 islands were inhabited. The entire population of all these islands some say could be squeezed into the Rose Bowl.

William A. Lessa wrote: In 1838, the French explorer Dumont D'Urville divided up the Pacific into Polynesia, Melanesia, and Micronesia. Scholars since then have debated whether or not these three terms do justice to the diversity of cultures in these areas, especially in Micronesia, where the first settlers arrived at various times and brought with them different cultures and languages. The Micronesians' exposure to Western influences also varied. The people of the Marianas, for example, were Christianized by the Spanish by 1700 ce. The Caroline island of Ifalik, on the other hand, became Christian only after World War II. [Source: William A. Lessa (1987), Encyclopedia of Religion, Encyclopedia.com. Lessa (1908-1997) taught at the University of California, Los Angeles (UCLA) and is regarded as "one of the pillars of anthropology in Micronesia", Lessa is best known for his work on Ulithi Atoll in Micronesia.]

Islands

Ocean islands are basically divided into three types: 1) "low" coral and sand islands; 2) "high" islands (usually exposed peaks and ridge-tops of submerged mountains and volcanos); and 3) parts of the continental shelf. Some continental islands were mountains and hills along the coast during last Ice Age when ocean levels were lower.

Low islands or cays were formed on coral shoals from reef sediments. Atoll islands are low islands (See Below). Seabird dropping fertilize the soils of some of these islands, which allow scrubby forest to take root. Others are battered regularly by storms and are little more than shifting piles of sand. Some patches of sand are so low they disappear during low tide and lose their status as islands.

High islands generally have better soil and a better supply of water than low islands. Low islands support only a few species of plant because there little topsoil and this soil has a high salt content. Although they often have no visible water sources they often are positioned over water lenses that trap rain water and can provide fresh water through wells.

Image Sources:

Text Sources: CIA World Factbook, 2023; “Encyclopedia of World Cultures, Volume 2: Oceania,” edited by Terence E. Hays, 1991, Wikipedia, New York Times, Washington Post, Los Angeles Times, Times of London, Lonely Planet Guides, Library of Congress, The Guardian, National Geographic, Smithsonian magazine, The New Yorker, Reuters, Associated Press, AFP, BBC, CNN, and various books, websites and other publications.

Last updated August 2023


This site contains copyrighted material the use of which has not always been authorized by the copyright owner. Such material is made available in an effort to advance understanding of country or topic discussed in the article. This constitutes 'fair use' of any such copyrighted material as provided for in section 107 of the US Copyright Law. In accordance with Title 17 U.S.C. Section 107, the material on this site is distributed without profit. If you wish to use copyrighted material from this site for purposes of your own that go beyond 'fair use', you must obtain permission from the copyright owner. If you are the copyright owner and would like this content removed from factsanddetails.com, please contact me.