Madagascar
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Where is Madagascar located?
Madagascar is an island country located off the southeastern coast of Africa, in the southwestern Indian Ocean. It is separated from the African coast by the Mozambique Channel. Madagascar is the fourth largest island in the world. The capital of Madagascar is Antananarivo.
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What makes Madagascar unique among the world's islands?
Madagascar's unique characteristics arise from its geographic isolation and distinctive blend of Asian and African cultural elements. Separated from the African coast by the Mozambique Channel, the island evolved as a separate physical and biological entity.
Many of Madagascar's plant and animal species are endemic, including about 40 species of lemurs. The Malagasy language, though geographically close to Bantu-speaking Africa, is of Western Malayo-Polynesian origin, demonstrating a unique cultural combination. Known as the Great Red Island, Madagascar possesses a diverse landscape, from rainforests to deciduous forests and spiny thickets.
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What are some famous animals that live only in Madagascar?
Madagascar's geographic isolation has led to a diverse array of endemic species. The island is home to nearly 40 species of lemurs, like the ring-tailed lemur, recognized by its striped tail. The fossa, Madagascar's largest native carnivore, is a cat-like animal that preys on lemurs and other small animals. Another notable endemic species is the tomato frog, a red, plump frog that secretes a white, glue-like substance to deter predators.
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What languages are spoken by people in Madagascar?
In Madagascar, the national language is Malagasy, a standardized version of Merina, an Austronesian language. Though geographically close to Bantu-speaking Africa, Malagasy contains Bantu words and phonetic and grammatical modifiers of Bantu origin.
French is also widely spoken and officially recognized. It serves as a medium of instruction, especially in upper grades, alongside Malagasy. Additionally, English is spoken, with increasing use, and Comorian is spoken among a sizable community of immigrants from Comoros.
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How did Madagascar's history shape its culture?
Madagascar's culture is a unique blend of Asian and African influences, evident in its language, social structures, and traditions. The Malagasy language, though geographically close to Bantu-speaking Africa, originates from the Western Malayo-Polynesian branch of the Austronesian language family, indicating Indonesian origins.
The island's history of settlement and political evolution has shaped its social divisions, with distinctions between the plateau and coastal peoples. The Merina kingdom's rise in the central plateau and subsequent conquest of the island established a ruling elite, further influencing social and economic dynamics. Despite these divisions, Madagascar's culture reflects a unique blend of Asian and African features.
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What environmental challenges does Madagascar face today?
Madagascar faces several environmental challenges today, including deforestation, which has significantly reduced the island's forest cover due to clearing for rice fields, fuel, building materials, and valuable timber exports. The widespread practice of slash-and-burn agriculture for temporary land clearance further exacerbates this issue. This has led to serious erosion and degradation of the land, with many original plant species lost. Illegal fishing and overfishing also threaten Madagascar's rich marine wildlife, creating additional environmental concerns.
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News •
Madagascar, island country lying off the southeastern coast of Africa. Madagascar is the fourth largest island in the world, after Greenland, New Guinea, and Borneo.
Although located some 250 miles (400 km) from the African continent, Madagascar’s population is primarily related not to African peoples but rather to those of Indonesia, more than 3,000 miles (4,800 km) to the east. The Malagasy peoples, moreover, do not consider themselves to be Africans, but, because of the continuing bond with France that resulted from former colonial rule, the island developed political, economic, and cultural links with the French-speaking countries of western Africa. The animal life and vegetation of the island are equally anomalous, differing greatly from that of nearby Africa and being in many respects unique. Although the coastlands have been known to Europeans for more than 400 years and to Arabs for much longer, recent historical development has been more intense and concentrated in the central plateau, which contains the capital city of Antananarivo (formerly Tananarive).
- Head Of Government:
- Prime Minister: Mamitiana Rajaonarison
- Capital:
- Antananarivo
- Population:
- (2026 est.) 32,659,000
- Head Of State :
- President: Col. Michael Randrianirina
- Form Of Government:
- transitional military government1 with two legislative houses (Senate [18]2; National Assembly [163])
- Official Languages:
- Malagasy; French3
- Official Religion:
- none
- Official Name:
- Repoblikan’i Madagasikara (Malagasy); République de Madagascar (French) (Republic of Madagascar)
- Total Area (Sq Km):
- 591,896
- Total Area (Sq Mi):
- 228,532
- Monetary Unit:
- ariary (MGA)
- Population Rank:
- (2026) 51
- Population Projection 2030:
- 33,417,000
- Density: Persons Per Sq Mi:
- (2026) 142.9
- Density: Persons Per Sq Km:
- (2026) 55.2
- Urban-Rural Population:
- Urban: (2018) 19.3%
- Rural: (2018) 80.7%
- Life Expectancy At Birth:
- Male: (2021) 65.8 years
- Female: (2021) 69.7 years
- Gni (U.S.$ ’000,000):
- (2024) 16,429
- Gni Per Capita (U.S.$):
- (2024) 510
- After a period of unrest, Col. Michael Randrianirina declared the military had taken power on October 14, 2025. The High Constitutional Court asked him to temporarily serve as president and organize new elections within 60 days, but a transitional administration that would govern for up to two years was established, and Randrianirina was inaugurated as president on October 17.
- Senate elections scheduled for December 11, 2025, were canceled, and the Senate term expired on January 18, 2026. On January 19, the High Constitutional Court ruled that the National Assembly alone would exercise legislative power until a new Senate was in place.
- Per the 2010 constitution.
Land
Madagascar is located in the southwestern Indian Ocean and is separated from the African coast by the 250-mile- (400-km-) wide Mozambique Channel.
Relief
Madagascar consists of three parallel longitudinal zones—the central plateau, the coastal strip in the east, and the zone of low plateaus and plains in the west.
Situated between 2,500 and 4,500 feet (800 and 1,400 metres) above sea level, the plateau has been uplifted and worn down several times and is tilted to the west. Three massifs are more than 8,500 feet (2,600 metres) high. The Tsaratanana region in the north is separated from the rest of the plateau by the Tsaratanana Massif, whose summit, Maromokotro, reaches 9,436 feet (2,876 metres) and is the highest point on the island. Ankaratra Massif in the centre is an enormous volcanic mass whose summit, Tsiafajavona, is 8,671 feet (2,643 metres) high. Ankaratra is a major watershed divide separating three main river basins. Farther south, Andringitra is a vast granite massif north of Tôlan̈aro (Faradofay); it rises to 8,720 feet (2,658 metres) at Boby Peak.
The plateau slopes with some regularity toward the extreme southern plain, but its boundaries to the east and west are more abrupt. To the east it descends in a sharp fault, by vertical steps of 1,000 to 2,000 feet (300 to 600 metres). This cliff, which is called the Great Cliff or the Cliff of Angavo, is often impassable and is itself bordered by the Betsimisaraka Escarpment, a second and lower cliff to the east, which overhangs the coastal plain. Behind the scarp face are the remains of ancient lakes, including one called Alaotra. To the south the two steep gradients meet and form the Mahafaly and the Androy plateaus, which overhang the sea in precipitous cliffs. Toward the west the descent is made in a series of steps. However, in places the central plateau is bordered by an impassable escarpment, such as the Cliff of Bongolava in the west-central part of the island. To the extreme north the plateau is bordered by the low belt of the Ambohitra Mountains, which include a series of volcanic craters.
The coastal strip has an average width of about 30 miles (50 km). It is a narrow alluvial plain that terminates in a low coastline bordered with lagoons linked together by the Pangalanes (Ampangalana) Canal, which is more than 370 miles (600 km) long. To the south of Farafangana the coast becomes rocky, and in the southeast there occur many little bays. To the northeast is the deep Bay of Antongil (Antongila).
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The western zone is between 60 and 125 miles (100 and 200 km) wide. Its sedimentary layers slope toward the Mozambique Channel and produce a succession of hills. The inland (eastern) side of these steep hills dominates the hollows formed in the soft sediments of the interior, while the other side descends to the sea in rocky slopes. The coastline is straight, bordered by small dunes and fringed with mangroves. The currents in the Mozambique Channel have favoured the offshore deposit of alluvium and the growth of river deltas. On the northwestern coast there are a number of estuaries and bays. This coast is bordered by coral reefs and volcanic islands, such as Nosy Be (Nossi-Bé), which protects Ampasindava Bay.
Drainage
The steep eastern face of the plateau is drained by numerous short, torrential rivers, such as the Mandrare, the Mananara, the Faraony, the Ivondro, and the Maningory, which discharge either into the coastal lagoons or directly into the sea over waterfalls and rapids. The more gently sloping western side of the plateau is crossed by longer and larger rivers, including the Onilahy, the Mangoky, the Tsiribihina, and the Betsiboka, which bring huge deposits of fertile alluvium down into the vast plains and many-channeled estuaries; the river mouths, while not completely blocked by this sediment, are studded with numerous sandbanks.
There are many lakes of volcanic origin on the island, such as Lake Itasy. Alaotra is the last surviving lake of the eastern slope. Lake Tsimanampetsotsa, near the coast south of Toliara (formerly Tuléar), is a large body of saline water that has no outlet.
Soils
The central plateau and the eastern coast are mainly composed of gneiss, granite, quartz, and other crystalline rock formations. The gneiss decomposes into red murrum, laterite, and deeper and more fertile red earths, giving Madagascar its colloquial name the Great Red Island. Fertile alluvial soils in the valleys support intensive cultivation. There also are scattered volcanic intrusions that produce fertile but easily erodible soils. Lake Alaotra is a large sedimentary pocket in the central plateau containing some of the island’s most productive farmland. The western third of the island consists entirely of deposits of sedimentary rock, giving rise to soils of medium to low fertility.