Australia and Oceania facts and geographical maps - World

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Australia and Oceania facts and geographical maps

Geographical facts about Australia and Oceania. Maps of Australia and Oceania
The main geographical facts about Australia and Oceania - population, country area, capital, ethnic groups, official language, religions, industry and culture. Maps of Australia and Oceania with cities
Oceania geography facts file
Regions of the World - Oceania
Oceania is the name given to a group of islands spread over 8.5 million sq km (3.3 million sq miles) in the Pacific Ocean, the majority of which lie in the southern hemisphere. The islands range in size from the large island continent of Australia, through medium-sized nations such as Papua New Guinea and New Zealand, to much smaller countries, such as Vanuatu and Tonga.
On cultural grounds, the islands can be divided into four groups. The first, Micronesia, lies east of the Philippines and includes the Federated States of Micronesia, Palau, the Marshall Islands, Nauru, and the USA dependencies of Guam and the Northern Mariana Islands. Melanesia, the second group, lies east of Indonesia and Australia, and includes Papua New Guinea, the Solomon Islands, Vanuatu, Fiji, Tonga, Tuvalu, and Samoa and the dependencies of New Caledonia (France) and American Samoa. Polynesia, the third, lies in the center of the Pacific Ocean, and includes Kiribati, French Polynesia, and the dependencies of Niue, the Cook Islands (NZ), the Pitcairn Islands (UK), and Hawaii (part of the USA). The fourth group comprises Australia and New Zealand. Unlike the other groups, these islands have indigenous populations, but the majority of the population are people who have migrated from Europe over the last two centuries. Australian dependencies include Norfolk Island in the Pacific Ocean and the Cocos (Keeling) and Christmas Islands in the Indian Ocean.
Physical features Oceania
Physiographically, the islands of Oceania can be classed into four categories. First there is Australia, situated in the middle of the Indo-Australian Plate, where there was no mountain building during the Tertiary geological era. Australia's eastern high-lands, the eroded remnants of old mountains, are a series of elevated plateaus; the western half of the country is an ancient eroded plateau linked to the east by vast sedimentary basins.
In the second category are the islands lying along the collision boundaries between crustal plates. In the South Pacific, New Zealand, Papua New Guinea, the Solomon Islands, and Fiji are within the collision zone between the Indo-Australian and the Pacific plates. In the North Pacific, the Mariana Islands lie along the collision boundary of the Eurasian and Pacific plates. These collisions have produced folded mountain ranges. New Zealand and Papua New Guinea have young mountain ranges, some peaks exceeding 3,000 m (10,000 ft).
The third category includes volcanic islands such as Fiji, which rise from the floor of the Pacific Ocean basin. Much smaller than the countries in the second category, they are mostly made up of high mountains, with some low-lying fringes along the coastlines, including coral reefs.
Finally, there are coral islands and atolls, such as Tuvalu. Atolls form low-lying circular coral reefs which enclose lagoons. The atolls typically develop around submerged volcanic cones. In some places, such as in Guam, coral islands have been raised by crustal movements.
Climate and vegetation Oceania
Oceania can be divided into two climatic zones: temperate and tropical. A large part of Australia and all of New Zealand lie in the temperate zone, while most of the island countries of the Pacific are tropical. Persistent trade winds dominate much of Oceania, and tropical cyclones often cause considerable damage.
Large parts of Australia are arid or semiarid. Humid zones are found along most of the east coast and Tasmania, and in part of the northern coast during summer. Most of New Zealand, Papua New Guinea and most of the islands in the Pacific are humid. However, droughts associated with the El Nino phenomenon have been frequent in recent decades in northern Australia and Papua New Guinea. Rainforests, both tropical and temperate, occur in all the humid regions of Oceania— Australia and the larger and high (mostly volcanic) islands. However, deforestation has taken place in several places, such as parts of eastern Australia, Tasmania, New Zealand, and the Solomon Islands.
The kangaroo, probably Australia's most well known native animal. While some such animals are threatened with extinction, kangaroos are in fact regarded as pests by many.
Isolation has been a major factor in the development of unique species of animals, birds, and plants in the Pacific islands. The spread of human habitation and hunting has seriously affected native animals, especially in Australia—several species are extinct or endangered.
Population Oceania
In 2000 the population of Oceania totalled 31 million. Australia and New Zealand accounted for 22.4 million people and Papua New Guinea for 4.7 million people. The remaining 3-9 million inhabitants are scattered on many small islands over a large area. Life expectancy for the area as a whole is 71.8 years for males and 76.6 for females. The annual population growth rate averages 1.2 percent but this varies widely, with one percent for Australia and New Zealand, 2.4 percent for Papua New Guinea, and 2.1 percent for Melanesia. Rates of urbanization vary widely too, being 89 percent for Australia and New Zealand and 17.4 percent for Papua New Guinea.
Agriculture Oceania
Agriculture in Oceania can be divided into three kinds: labor-intensive subsistence agriculture, which occurs in most of the tropical islands of the Pacific; plantation crops, which are cultivated in the medium-sized tropical islands; and capital-intensive agriculture, which is found in Australia and New Zealand.
Subsistence agriculture in the Pacific islands consists of short-life items such as cassava, taro, yams, breadfruit, and sweet potatoes. Bananas and papayas are the most commonly grown fruits. Coconut palms grow on almost all the islands, and are a source of fresh food. Oil is extracted from the dried coconut meat (copra). Copra is exported from countries such as Vanuatu and Samoa. Cash crops, often a legacy of colonial times, are also important in some of the Pacific nations—sugar in Fiji and cocoa in Vanuatu.
Fishing is important for the majority of Pacific islands, as their economic zones extend to the 200 nautical mile limit—a large area compared to the size of many of the islands. Several islands have granted fishing licenses to Japanese, South Korean, and Taiwanese companies.
Industrialization Oceania
Australia and New Zealand both have modern diversified economies with well-established infrastructures. Australia is particularly well favored as it has rich mineral deposits and energy sources. Manufacturing, including food processing, makes an important contribution to the economy of these two Pacific nations.
In contrast, the other islands of the Pacific are not industrially developed. Papua New Guinea, is rich in minerals such as copper and gold, and has recently discovered natural gas fields. There are nickel deposits in New Caledonia and gold in Fiji, both of which are exported rather than used in local industries.
Many islands in the Pacific have few resources; some have insufficient land for their people and a number lack adequate supplies of drinking water. This shortage of natural resources, coupled with poor infrastructures, has impeded industrial development. Industry in most of the islands is limited to food processing.
Tourism has become an important source of revenue for much of Oceania. Australia and New Zealand offer tourists modern amenities and facilities, while the beautiful scenery of tropical Pacific Islands like Fiji, Tahiti, Vanuatu, and the Northern Mariana Islands attract visitors.
Languages Oceania
Culturally, Oceania can be divided into two major groups: the predominantly European settlements of Australia and New Zealand, and Melanesia, Polynesia, and Micronesia, which have been long settled by Oceanic peoples. New Caledonia is partially settled by Europeans.
During the colonial era, the entire region came under European influence. This resulted in English and French becoming important languages, depending on the colonial powers (Britain, America, and France). English is the official language of New Zealand, Australia, Papua New Guinea, the Solomon Islands, Vanuatu, and Fiji. French is
spoken in New Caledonia and French Polynesia. On several of the Pacific islands, particularly Papua New Guinea and Vanuatu, pidgin is a common lingua franca.
In Australia, only remnants of the numerous Aboriginal languages that were spoken in the continent before European settlement still exist. Several of these languages are found in the Northern Territory and the northern part of Western Australia (the Kimberleys), where Walmadjeri is becoming a common language among several Aboriginal tribes. In New Zealand, which has a significant Maori population, the Maori language is widely spoken.
Numerous languages are found in Melanesia, Polynesia, and Micronesia. In Papua New Guinea, hundreds of languages are spoken, Austronesian languages being spoken along the coastline and Papuan languages in the highlands. Austronesian languages such as Fijian in Fiji and Tahitian, Ton-gan, and Samoan in Polynesia are widespread.
Boundary disputes and wars Oceania
The whole region was affected by the Japanese invasion during the Second World War, and was the site of many important battles. No significant boundary disputes exist in the region. In recent decades, boundaries have been drawn up for Oceanic economic zones. However, there have been civil disturbances in both Fiji and New Caledonia—the former related to the struggle for a less racially biased government in the years after Fiji became a republic in 1970, the latter related to the wish of some of the people to become independent from France.
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