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    Papua New Guinea (pronounced /ˈpæpuːə njuː ˈgɪni/, /ˈpæpjuːə/ ), in Tok Pisin : Papua Niugini , officially the Independent State of Papua New Guinea , is a country in ...

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    Papua New Guinea " is a 1991 song by the electronic music group Future Sound of London . It was the group's debut single and later appeared on their full-length album Accelerator ...

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    With the overarching objective of alleviating poverty, ADB strategy for Papua New Guinea focuses on strengthening governance, supporting private sector development, and improving ...

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Papua New Guinea

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I

Introduction

Papua New Guinea, independent nation in the southwestern Pacific Ocean, located north of Australia and east of Indonesia. Papua New Guinea occupies the eastern half of the island of New Guinea, called the mainland, and several hundred smaller islands. The western part of New Guinea forms the Indonesian province of Papua (formerly Irian Jaya). Most Papua New Guineans live in rural villages along the coast or in the rugged interior. High mountains and rain forests isolate many villages, although a network of roads and airstrips serves mines and plantations. Since the country’s independence from Australia in 1975, town and city life has expanded as villagers have migrated to urban areas in search of employment. Port Moresby, located on the mainland’s southeastern coast, is Papua New Guinea’s capital and largest city.

II

Land and Resources

Papua New Guinea has a total area of 462,840 sq km (178,704 sq mi), of which nearly 90 percent is on the mainland. The smaller islands of Papua New Guinea all lie to the east and north. Among them are the Bismarck Archipelago, which includes New Britain, New Ireland, and Manus; the northern part of the Solomon Islands, including Bougainville and Buka; the Louisiade Archipelago; the Trobriand Islands; and the D’Entrecasteaux Islands.

A

Physical Features

The mainland, which is wide in western Papua New Guinea and narrows in the southeast, has a rugged, mountainous interior. Steep slopes and jagged peaks stretch across the entire island from east to west. In Papua New Guinea, the mountains rise to a maximum elevation of 4,509 m (14,793 ft) at Mount Wilhelm in the Bismarck Range. Among the other ranges is the Owen Stanley in the southeast. Between the mountains are broad valleys that lie more than 1,500 m (4,900 ft) above sea level. These mountains and valleys constitute the central highlands. To the north of the central highlands is a low-lying, swampy plain. It was formed by sediment deposited by large rivers, including the Sepik and Ramu, which flow from the mountains into the Bismarck Sea. North of this plain are other mountain ranges that fringe the island’s coast. These run from west to east and continue in scattered peaks offshore, forming the islands of New Britain, New Ireland, and Bougainville. Most of the other large islands are mountainous. A few islands, such as the Trobriands, are low coral formations.

The coastline of mainland Papua New Guinea is mostly low-lying. In the south it is deeply indented by river mouths and by a number of bays, such as Milne Bay at the eastern extremity. Most southward-flowing rivers empty into the Gulf of Papua. Major rivers of the mainland include the Fly, in the southwest; the Purari and Kikori, in the south; and the Sepik and Ramu, in the north. The Fly is navigable for about 800 km (about 500 mi) and the Sepik for about 500 km (about 300 mi).



Papua New Guinea lies along the so-called Ring of Fire, a belt of frequent tectonic activity in the Pacific Ocean caused by the collision of several continental plates (see Plate Tectonics). The country often experiences earthquakes and there are about 40 active volcanoes along the north coast of the mainland and on the smaller islands. Dramatic examples of tectonic activity include the 1951 eruption of Mount Lamington on the mainland and volcanic eruptions and earthquakes in 1937 and 1994 near Rabaul in eastern New Britain. The latter event, which the government described as the nation’s worst recorded natural disaster, caused the evacuation of about 90,000 people.

B

Plants and Animals

Three-quarters of Papua New Guinea has retained its natural vegetation, which is mainly dense rain forest. Sago palms and mangrove swamps cover parts of the mainland coast. Farther inland are tropical rain forests and grasslands. The mountainous areas also contain stands of pine trees and deciduous forests, and the tops of some mountains have alpine vegetation.

Papua New Guinea’s wild animal life is abundant and varied. The majority of animals are similar to those found in Australia, but there are many species of both animals and plants that exist only in Papua New Guinea and Papua. Monotremes (egg-laying mammals) such as echidnas (spiny anteaters) are among the mammals commonly found on the island, as are marsupials, including tree kangaroos, wallabies, and phalangers. Wild pigs, rats, bats, and mice are also common mammals, some of which were introduced by early human immigrants. Papua New Guinea also has hundreds of species of tropical birds, among them many unique and protected birds of paradise. Reptile species, including snakes, lizards, and the New Guinea crocodile, are numerous. A number of crocodile farms export skins and sell the meat. Insects abound, including large and colorful butterfly species and malaria-carrying Anopheles mosquitoes. The coastal waters support many species of fish, shellfish, and turtles.

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