Geography of the Maldives

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Maldives is a country of South Asia, situated in the Indian Ocean, south-southwest of India. It consists of approximately 1,196 coral islands grouped in a double chain of 27 atolls, spread over roughly 90,000 square kilometers, making this one of the most disparate countries in the world. Composed of live coral reefs and sand bars, the 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.

The largest island of Maldives is Fuvammulah, which is a single island and single atoll located in the southern part of the Maldives known as Gnaviyani Atoll in the administrative division. In Addu Atoll the westernmost islands are connected by roads over the reef and the total length of the road is 12 km.

Geographic coordinates: 3°15′N 73°00′E

Contents 1 Physiography 2 Climate 3 Area and boundaries 4 Resources and land use 5 Environmental concerns 6 Other facts 7 See also 8 References 9 External links

[edit] Physiography

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 50 kilometers long from north to south, and 30 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 20 to 60. 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 Fuvammulah 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 26 km², is cultivated with taro, bananas, coconuts, and other fruit. Only the lush island of Fuvammulah produces fruits such as oranges and pineapples partly because the terrain of Fuvammulah 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.

[edit] Climate

The temperature of Maldives ranges between 24 and 33 °C throughout the year. Although the humidity is relatively high, the constant sea breezes help to keep the air moving. Two seasons dominate Maldives' weather: the dry season associated with the winter northeast monsoon and the rainy season brought by the summer southwest monsoon. The annual rainfall averages 2,540 millimeters in the north and 3,810 millimeters in the south.

The weather in Maldives is affected by the large landmass of the South Asia to the north. The presence of this landmass causes differential heating of land and water. Scientists also cite other factors in the formation of monsoons, including the barrier of the Himalayas on the northern fringe of the South Asia and the sun's northward tilt, which shifts the jet stream north. These factors set off a rush of moisture-rich air from the Indian Ocean over the South Asia, resulting in the southwest monsoon. The hot air that rises over the South Asia during April and May creates low-pressure areas into which the cooler, moisture-bearing winds from the Indian Ocean flow. In Maldives, the wet southwest monsoon lasts from the end of April to the end of October and brings the worst weather with strong winds and storms. In May 1991 violent monsoon winds created tidal waves that damaged thousands of houses and piers, flooded arable land with seawater, and uprooted thousands of fruit trees. The damage caused was estimated at US$30 million.

The shift from the moist southwest monsoon to the dry northeast monsoon over the South Asia occurs during October and November. During this period, the northeast winds contribute to the formation of the northeast monsoon, which reaches Maldives in the beginning of December and lasts until the end of March. However, the weather patterns of Maldives do not always conform to the monsoon patterns of the South Asia. Rain showers over the whole country have been known to persist for up to one week during the midst of the dry season.

[edit] Area and boundaries

Area:
total: 300 km²
land: 300 km²
water: 0 km²

Coastline: 644 km

Maritime claims: measured from claimed archipelagic baselines
contiguous zone: 24 nautical miles (44 km)
exclusive economic zone: 200 nautical miles (370 km)
territorial sea: 12 nautical miles (22 km)

Elevation extremes:
lowest point: Indian Ocean 0 m
highest point: unnamed location on Vilingili Island in the Addu Atoll 2.4 m (Maldives is the flattest country in the world, i.e. they have the lowest high-point of any country in the world).

[edit] Resources and land use

Natural resources: fish

Land use:
arable land: 10%
permanent crops: 0%
permanent pastures: 3%
forests and woodland: 3%
other: 84% (1993 est.)

Irrigated land: NA

[edit] Environmental concerns

Natural hazards: low level of islands makes them very sensitive to sea level rise

Environment - current issues: depletion of freshwater aquifers threatens water supplies; global warming and sea level rise; coral reef bleaching, overpopulation, deforestation, air pollution

Environment - international agreements:
party to: Biodiversity, Climate Change, Climate Change-Kyoto Protocol, Hazardous Wastes, Ozone Layer Protection
signed, but not ratified: Law of the Sea

[edit] Other facts

• Position: degree of latitude: 07° 06'30" N to 00° 41'48" S and degree of longitude: 72° 32'30" E to 73° 45'54" E westside of India and Sri Lanka.
• Range: in length approx. 750 km (from north to south) / in width approx. 120 km (from west to east)
• Land territory: 1,196 mostly deserted islands with a total area of approx. 298 km².
• The islands are very flat and are in average 1.8 m above sea level.
• Distances: shortest distance to India: approx. 340 km and to Sri Lanka approx. 700 km.

[edit] See also

• Atolls of the Maldives

[edit] References

• This article contains material from the Library of Congress Country Studies, which are United States government publications in the public domain.

[edit] External links

• Map of the Baa atoll
• Satellite images of all the Atolls

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