Sources: The Library of Congress Country Studies; CIA World Factbook
Maldives consists of approximately 1,200 coral islands grouped in a double chain of twenty-seven atolls. Composed of live coral reefs and sand bars, these atolls are situated atop a submarine ridge 960 kilometers long that rises abruptly from the depths of the Indian Ocean and runs from north to south. Only near the southern end of this natural coral barricade do two open passages permit safe ship navigation from one side of the Indian Ocean to the other through the territorial waters of Maldives. For administrative purposes the Maldives government organized these atolls into nineteen administrative divisions (see fig. 8; Government and Politics , this ch.).
Most atolls consist of a large, ring-shaped coral reef supporting numerous small islands. Islands average only one to two square kilometers in area, and lie between one and 1.5 meters above mean sea level. The highest island is situated at three meters above sea level. Maldives has no hills or rivers. Although some larger atolls are approximately fifty kilometers long from north to south, and thirty kilometers wide from east to west, no individual island is longer than eight kilometers.
Each atoll has approximately five to ten inhabited islands; the uninhabited islands of each atoll number approximately twenty to sixty. Several atolls, however, consist of one large, isolated island surrounded by a steep coral beach. The most notable example of this type of atoll is the large island of Fua Mulaku situated in the middle of the Equatorial Channel.
The tropical vegetation of Maldives comprises groves of breadfruit trees and coconut palms towering above dense scrub, shrubs, and flowers. The soil is sandy and highly alkaline, and a deficiency in nitrogen, potash, and iron severely limits agricultural potential. Ten percent of the land, or about 2,600 hectares, is cultivated with taro, bananas, coconuts, and other fruit. Only the lush island of Fua Mulaku produces fruits such as oranges and pineapples partly because the terrain of Fua Mulaku is higher than most other islands, leaving the groundwater less subject to seawater penetration. Freshwater floats in a layer, or "lens," above the seawater that permeates the limestone and coral sands of the islands. These lenses are shrinking rapidly on Male and on many islands where there are resorts catering to foreign tourists. Mango trees already have been reported dying on Male because of salt penetration. Most residents of the atolls depend on groundwater or rainwater for drinking purposes. Concerns over global warming and a possible long-term rise in sea level as a result of the melting of polar ice are important issues to the fragile balance between the people and the environment of Maldives in the 1990s.
Data as of August 1994
NOTE: The information regarding Maldives on this page is re-published from The Library of Congress Country Studies and the CIA World Factbook. No claims are made regarding the accuracy of Maldives Physiography information contained here. All suggestions for corrections of any errors about Maldives Physiography should be addressed to the Library of Congress and the CIA.