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Independence Day of the Independent State of Samoa

Samoa, country in the central South Pacific Ocean, among the westernmost of the island countries of Polynesia.

According to legend, Samoa is known as the “Cradle of Polynesia” because Savai‘i island is said to be Hawaiki, the Polynesian homeland. Samoan culture is undoubtedly central to Polynesian life, and its styles of music, dance, and visual art have gained renown throughout the Pacific islands and the world. The country’s international image is that of a tropical paradise inhabited by tourist-friendly flower-wreathed peoples. Yet this belies the economic, social, and political challenges of this diverse and evolving Pacific microstate. Samoa gained its independence from New Zealand in 1962 after more than a century of foreign influence and domination, but it remains a member of the Commonwealth. The country was known as Western Samoa until 1997. Its capital and main commercial centre is Apia, on the island of Upolu.


Samoa lies approximately 80 miles (130 km) west of American Samoa, 1,800 miles (2,900 km) northeast of New Zealand, and 2,600 miles (4,200 km) southwest of Hawaii. Samoa, which shares the Samoan archipelago with American Samoa, consists of nine islands west of longitude 171° W—Upolu, Savai‘i, Manono, and Apolima, all of which are inhabited, and the uninhabited islands of Fanuatapu, Namu‘a, Nu‘utele, Nu‘ulua, and Nu‘usafee. (The six Samoan islands east of the meridian are part of American Samoa.) The total land area is smaller than the U.S. state of Rhode Island but about 2.5 times larger than Hong Kong.

Relief and drainage

Savai‘i, the largest island, covers 659 square miles (1,707 square km) and rises to a maximum elevation of 6,095 feet (1,858 metres) at Mount Silisili, a volcano at the island’s approximate centre. Mounts Māfane, Mata‘aga, and Maugaloa are also imposing peaks. Upolu, the other large island, lies about 10 miles (16 km) to the east across the Apolima Strait. Upolu is more elongated and uneven in shape than Savai‘i and has lower average elevations. It occupies an area of 432 square miles (1,119 square km), including five offshore islets, and rises to 3,608 feet (1,100 metres) at Mount Fito. Manono and Apolima are smaller islands lying in the strait between the two main islands.

All the country’s rivers are shallow, are limited in extent, and radiate directly from the central highlands to the coast. The islands are rocky, formed by volcanic activity that progressed from east to west within the past seven million years. They are ringed by coral reefs and shallow lagoons except where the shorelines are marked by cliffs formed by lava flows. Mount Matavanu on Savai‘i last erupted intermittently during 1905–11. Samoa’s volcanic soils support lush vegetation but are easily eroded by runoff.


The climate is tropical and humid. Precipitation varies from more than 100 inches (2,540 mm) on the northern and western coasts to 300 inches (7,620 mm) inland. Temperatures vary little, averaging 80 °F (27 °C) and ranging between 73 and 86 °F (23 and 30 °C) throughout the year. The southeast trade winds prevail, varying occasionally to northerlies during the wet season (November or December to April), when severe storms are liable to occur. Typhoons occasionally cause widespread damage.

Plant and animal life

Samoa’s lush vegetation includes inland rainforests and cloud forests. Large sections of the coast have been covered with taro plantations and coconut groves. The islands support limited animal life, although more than 50 species of birds are found there, at least 16 of them indigenous, including rare tooth-billed pigeons. The only native mammals are flying foxes, which are endangered, and other species of smaller bats. Rats, wild cattle, and pigs have been introduced. Among the smaller animals found in Samoa are several species of lizards, two snakes of the boa family, centipedes and millipedes, scorpions, spiders, and a wide variety of insects.

O Le Pupu Pue National Park (1978), Samoa’s first national park, occupies some 11 square miles (28 square km) on south-central Upolu. Conservation efforts have been lax in many Samoan communities. Soil erosion, resulting from farming steep slopes and clear-cutting forests, has produced runoff that has damaged many of Samoa’s lagoons and coral reefs. Industrial and residential pollution has become a concern in and around Apia. Wildfires in 1998, which were started by farmers clearing land for cultivation, destroyed nearly one-fourth of the forests on Savai‘i.

People of Samoa

Ethnic groups

Samoans are mainly of Polynesian heritage, and about nine-tenths of the population are ethnic Samoans. Euronesians (people of mixed European and Polynesian ancestry) account for most of the rest of the population, and a tiny fraction are of wholly European heritage.


Samoan is the country’s official language; legislative activity is conducted in both Samoan and English as required by the constitution. Samoan is believed to be among the oldest of the Polynesian tongues and is closely related to the Maori, Tahitian, Hawaiian, and Tongan languages. A large number of Samoan words reflect maritime traditions, including names for ocean currents, winds, landforms, stars, and directions. Some verb forms indicate the relative positions of objects, including directions of movement toward or away from the speaker. English is widely spoken as a second language.


Samoans traditionally had a pantheistic religion, where family elders performed most rituals; they appear not to have had a dominant priestly class. They readily adopted Christian teachings following European contact, and even the more remote villages built churches, often of grand proportions. The Congregational Christian Church of Samoa (Ekalesia Faapotopotoga Kerisiano Samoa [EKFS]; formerly the London Missionary Society) is the dominant religion, with slightly less than one-third of the population. Approximately one-fifth of Samoans are Roman Catholics, and Latter-day Saints constitute about one-sixth of the population. Methodists make up one-eighth. Pentecostals, Assemblies of God, and other Christian groups have more-limited memberships.

Demographic trends

The birth rate in Samoa has been high since the 1950s, when the population reached about 80,000. Although that number had doubled by the mid-1990s, the population’s rate of increase remained markedly lower than the world average because tens of thousands of Samoans had emigrated to New Zealand, the United States, Australia, and elsewhere. Life expectancy at birth is 67 years for males and 72 for females. About one-third of Samoans are less than 15 years old.


Close kinship ties within the villages traditionally bound Samoans into a collectivist society, but a cash economy developed following European contact, mainly based on agricultural exports. Tourism, services, and light manufacturing became increasingly important after 1950. Other major sources of capital now include remittances from Samoans living abroad (mainly in the United States and New Zealand), which account for as much as one-sixth of household income, and grants from the United States, the United Nations, the Commonwealth, and other foreign entities.

Agriculture, forestry, and fishing

Agriculture accounts for two-fifths of Samoa’s gross domestic product (GDP) and nearly two-thirds of the workforce; however, production does not meet local demand, and large quantities of food are imported. Major crops include coconuts, taro, pineapples, mangoes, and other fruits. Typhoons caused widespread damage in the 1990s to several crops, including taro, which was also devastated by taro leaf blight. Cattle, pigs, and poultry are raised for local consumption. Forestry has made increasing contributions to the economy, partly because of the government’s replanting programs. The Samoan fishing industry remains small, based primarily on catches made from outrigger canoes.

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Source: https://www.britannica.com/place/Samoa-island-nation-Pacific-Ocean/People


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