Quick Facts
Born:
December 12, 1949, Imerikasina, Madagascar, French Union [now Madagascar] (age 75)

Marc Ravalomanana (born December 12, 1949, Imerikasina, Madagascar, French Union [now Madagascar]) is a Malagasy entrepreneur and politician who served as president of Madagascar (2002–09). He stepped down in the midst of a political crisis in 2009 and went into exile before returning in 2014. Ravalomanana was a candidate in Madagascar’s 2018 and 2023 presidential elections.

Early life and political career

Ravalomanana had a Protestant education, first by missionaries in his native village of Imerikasina, near Antananarivo, and then at a Protestant secondary school in Sweden. Returning to Antananarivo, he launched a family venture selling homemade yogurt, which quickly grew into a booming business. In less than two years, with assistance from the Protestant church, he secured a loan from the World Bank to purchase his first factory, and he soon had a monopoly of dairy and oil products. His company, TIKO, would become the largest domestically owned business in Madagascar.

Ravalomanana became politically active and was elected mayor of Antananarivo in 1999. While serving in this post, he gained the reputation as a bold manager. He balanced the city’s budget while embarking on a massive urban-restoration project, though he was criticized because some houses bulldozed during the operation were still being lived in. Under his administration, the city’s waste-disposal services and water quality also improved.

Undated photograph of Julius Nyerere, the first prime minister of Tanganyika, which eventually became Tanzania.
Britannica Quiz
Before They Were World Leaders: Africa Edition

2001 presidential election and crisis

In 2001 Ravalomanana challenged Didier Ratsiraka, the incumbent president for more than two decades, in the December presidential election. When the election results were made available, Ravalomanana’s lead over Ratsiraka appeared narrow enough to necessitate a runoff vote (required when neither candidate wins a majority). Ravalomanana, however, claimed that the results had been tampered with and that he was the clear winner—claims supported by observers—and demanded a recount. The recount was not immediately forthcoming, however, and the situation remained tense.

Ravalomanana enjoyed significant support, particularly in Antananarivo, where his supporters staged numerous demonstrations and launched a general strike in January 2002 that lasted for several weeks. When that was not enough to persuade the country’s High Constitutional Court—which had been padded with Ratsiraka’s appointees just prior to the election—to order a recount, Ravalomanana declared himself president. He held an inauguration on February 22 and began establishing his administration, despite the fact that the international community did not recognize him as the legitimate leader of the country and Ratsiraka still claimed the presidency. Ratsiraka’s administration fled to the port city of Toamasina (also known as Tamatave) and attempted to blockade Antananarivo, utilizing such tactics as blocking roads and destroying bridges to prevent the delivery of food and fuel into the city. His supporters fought with those of Ravalomanana, with each side eventually controlling various sections of the country.

In late April the High Constitutional Court (which had since had its preelection body of judges reinstated by the country’s Supreme Court) ruled that a recount proved Ravalomanana had indeed won more than 50 percent of the vote, but Ratsiraka would not accept the results of the recount. Nonetheless, Ravalomanana was inaugurated a second time on May 6, 2002. Supporters of each candidate continued to clash, though, as the country teetered on the cusp of civil war. Fighting between the two sides did not cease until midsummer, when Ravalomanana’s forces were able to take control over areas previously held by Ratsiraka’s supporters. International recognition of Ravalomanana’s government followed.

Presidency

Although the political crisis was over, Ravalomanana was faced with its aftermath: the country’s stability was precarious at best, and the economy was weakened. He promptly addressed the situation, implementing economic reforms and working tirelessly to entice foreign investors back to the country; his efforts won praise from foreign donors and international organizations. Ravalomanana also tried to foster a sense of national reconciliation. He created his own political party, I Love Madagascar (Tiako I Madagasikara; TIM), which did well in the December 2002 legislative elections. Ravalomanana was relatively popular in the early years of his term, though he still faced periodic unrest, including failed coup attempts in 2003 and 2006.

Are you a student?
Get a special academic rate on Britannica Premium.

In mid-2006 Ravalomanana announced that the presidential election would be held ahead of schedule in December of that year. Opposition groups were unable to field a strong candidate, and he was reelected with about 55 percent of the vote in an election that international observers generally considered free and fair. Ravalomanana’s popularity began to waver in some quarters in 2007, although his TIM party was able to maintain a strong majority of seats in the September 2007 legislative elections.

2009 political crisis and aftermath

In late 2008 Ravalomanana was challenged by Andry Rajoelina, the mayor of Antananarivo and a popular opposition leader. Rajoelina accused Ravalomanana of misappropriating public funds and ruling the country as a dictator and called for him to step down, which Ravalomanana refused to do. The struggle between Ravalomanana and Rajoelina came to a head in January 2009, when dozens were killed during opposition protests. Rajoelina was fired from his mayoral post, and the conflict between the two leaders developed into a tense stalemate with sporadic bouts of violence. The crisis intensified in March, when the head of the army was removed by a faction of troops who no longer supported Ravalomanana’s administration.

Although Ravalomanana had the support of the international community, domestically he was faced with the loss of military support and continued public unrest, and on March 17 he agreed to step down from office and hand power to the military. Within hours, military leaders transferred power to Rajoelina, who had already declared himself president. The international community widely condemned the military’s unconstitutional transfer of power to Rajoelina as a coup.

Ravalomanana went into exile on the African continent, but Madagascar was still left in the grips of political crisis, as Rajoelina was internationally shunned and did not have complete support of the Malagasy public. Over the next several months, Ravalomanana, along with Rajoelina and other Malagasy political leaders, participated in several mediation sessions led by international organizations in an attempt to alleviate the crisis. Rajoelina, however, rejected the outcome of these negotiations in late 2009. (For additional detail, see Madagascar: History, The Third Republic, Power Struggle.)

In August 2010 a Malagasy court convicted Ravalomanana in absentia of murder and sentenced him to life in prison with hard labor. The conviction was for the deaths of at least 30 of Rajoelina’s supporters that occurred when Ravalomanana’s presidential guard troops opened fire on protesters during a march on the presidential palace in February 2009; Ravalomanana rejected the verdict.

Although a new president, Hery Martial Rakotoarimanana Rajaonarimampianina, was inaugurated in January 2014, Ravalomanana remained in exile until October 2014. He was promptly detained by authorities after his arrival back in Madagascar and held without charges. In December he was permitted to return to his home, albeit under an order of house arrest. That order was not lifted until May 2015.

2018 and 2023 presidential elections

In the run-up to the 2018 presidential election, Ravalomanana stated his intention of being a candidate. However, new electoral laws championed by Rajaonarimampianina and passed in April 2018 prevented Ravalomanana’s candidacy on the basis of his 2010 conviction; they also introduced problems for other potential candidates. Ravalomanana’s supporters were joined by others in protesting the new electoral laws. After two protesters were killed by security forces, the demonstrations continued with the added purposes of denouncing the actions of the security forces and calling for Rajaonarimampianina’s resignation. In May the country’s High Constitutional Court struck down parts of the new laws, which led to the removal of the barriers to Ravalomanana’s candidacy in the upcoming presidential election, scheduled for November 7, 2018.

Ravalomanana was one of 36 candidates vying for the presidency, as were Rajoelina and Rajaonarimampianina. Ravalomanana came in second place in the November 7 poll, winning about 35 percent of the vote; he trailed Rajoelina, who garnered about 39 percent. With no candidate winning more than 50 percent, Ravalomanana faced Rajoelina in the December 19 runoff. He was defeated by Rajoelina, who captured more than 55 percent of the vote. Citing what he alleged were electoral flaws, Ravalomanana rejected the results and sought to have them cancelled by filing complaints with the High Constitutional Court. The court, however, rejected his complaints and upheld the election results.

Ravalomanana also ran for president in 2023. He placed third (behind winner Rajoelina and Siteny Randrianasoloniaiko) in the election, which had low voter turnout and was boycotted by the opposition.

The Editors of Encyclopaedia Britannica
This article was most recently revised and updated by Amy Tikkanen.

News

Kenya thrash Madagascar in Women's Rugby Africa Cup opener June 8, 2025, 10:38 PM ET (The Standard)

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).

Quick Facts
Madagascar
See article: flag of Madagascar
Audio File: National anthem of Madagascar
Head Of Government:
Prime Minister: Christian Ntsay
Capital:
Antananarivo
Population:
(2025 est.) 31,727,000
Head Of State :
President: Andry Rajoelina
Form Of Government:
republic with two legislative houses (National Assembly [151] and Senate [631])2
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):
228,531
Monetary Unit:
ariary (MGA)
Population Rank:
(2025) 51
Population Projection 2030:
33,417,000
Density: Persons Per Sq Mi:
(2025) 138.8
Density: Persons Per Sq Km:
(2025) 53.6
Urban-Rural Population:
Urban: (2018) 19.3%
Rural: (2018) 80.7%
Life Expectancy At Birth:
Male: (2022) 66.8 years
Female: (2022) 69.6 years
Literacy: Percentage Of Population Age 15 And Over Literate:
Male: (2022) 79%
Female: (2022) 76%
Gni (U.S.$ ’000,000):
(2023) 15,755
Gni Per Capita (U.S.$):
(2023) 510
  1. Forty-two are indirectly elected by an electoral college, and 21 are appointed by the head of state.
  2. A democratically elected president was inaugurated on January 25, 2014; the National Assembly was installed on February 18, 2014; a new prime minister was appointed on April 11, 2014; and the Senate was installed on December 29, 2015.
  3. Per the 2010 constitution.
Aidan William Southall

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.

7:023 Geography: Think of Something Big, globe showing Africa, Europe, and Eurasia
Britannica Quiz
Which Country Is Larger By Area? Quiz

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).

Are you a student?
Get a special academic rate on Britannica Premium.

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.

Jean Dresch

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.