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TAHITIAN CUSTOMS and CEREMONIES
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Ever since the Bounty landed on Tahiti,
An Islander is a person of the ocean who always has one foot in the water and the other on the land. The sea is like a tonic without which the Islanders cannot live happily - the sea is their life. The sea gives them their food and their tools are their canoes. Like their forefathers of old, the present day fishermen are skilled navigators and canoe builders who are addicted to the sea. They understand the moods of the sea; they are familiar with the stars and the sun, and they breathe inspiration from the prevailing trade winds. They are adventurous people who, like the seabirds, have the instinct to migrate in their blood. Their houses are a reflection of the pandanus and coconut trees from which they are constructed. The lifestyle is quite simple and in harmony with nature, living off the land and the sea.
The term Oceania is normally used to designate all the islands of the Central and the South Pacific including Australia (continent), New Zealand and sometimes the Malay Archipelago
it is important for us to always remember that Island life is really quite simple but is governed by very complex customs and rituals. These customs and rituals are a very important part of our lives from before we are born until after we die. They depict the great respect we have for our elders and ancestors and determine the way that they are treated, even after death. The customs and rituals give us the strength to cope in extreme hardship and when our environment is very hostile. They allow us to relate to the sea and all the creatures that live in the sea, and tell us that the sea, which provides us with our existence, can also be both our friend and enemy.
Island life may seem on the surface to be very idyllic but, in fact, our very existence is often very precarious. So many island communities live on small coral outcrops, often only a little above sea level. These outcrops can be very easily overtaken by the sea, however, despite all this, these atolls are our home and are inhabited by people with a great love for life. We are affectionate and friendly people who love laughing.
Air Tahiti
THE CENTRAL PACIFIC BASIN
The Pacific Ocean occupies nearly one-third of the earth's surface. One can sail across it along the equator, for a distance of 10,000 miles. From the Aleutian Islands on the north to the Antarctic continent on the south is a distance almost as great. The surface of the ocean has an area of about 65,000,000 square miles.
This ocean contains more than half of all the earth's volume of water, 165,000,000 cubic miles of it. The average depth of the Pacific Ocean is about 13,400 feet. The eastern half is of nearly uniform depth, averaging about 16,000 feet, and is rather free from islands. The western half has areas which are comparatively shallow alternating with narrow areas of very great depth, and there are numerous islands. One of the deep places (troughs), off the N.E. corner of Mindanao, Philippine Islands, contains the greatest depth yet sounded, 35,400 feet.
The central Pacific area contains ocean of rather uniform depth on its north-eastern side, and the remains of the ancient "Melanesian Continent" on its south-western side. Between are alternate ridges and troughs, most of which trend from northwest to southeast. Along the ridges are scattered chains of islands. Nearly parallel to each other, from north to south, we find: (1) the chain of Hawaiian Islands, (2) the Christmas-Palmyra chain, which may extend north-westward to Johnston Island, and to the southeast through the Marquesas Islands, (3) a ridge through Tongareva (Penrhyn) Island, which extends north-westward toward Baker and Howland Islands, and, after interruption, is continued south-eastward as the western Tuamotu Islands, (4) a ridge through Pukapuka and Nassau Islands, (after an interruption) through the Society Islands, and (after another break) through the eastern Tuamotu Islands, and (5) a ridge through the Samoan islands, and in line with it, one through the Cook and Austral Islands.
These ridges are great ranges of volcanic mountains rising from the bottom of the ocean. Where they protrude above the surface they form volcanic islands. In other places they have been carved off just below the surface and have been capped over with coral to form coral islands. Some of these form a ring around a central lagoon and are called atolls. Others have been pushed up to a height of several hundred, even a thousand feet, to form upraised coral islands. Coral reefs also may form around the margin of volcanic islands, or may surround them, at a little distance off shore to form barrier reefs.
Many millions of years ago perhaps hundreds of millions of years, a great mass of land extended south-eastward from the southeast corner of Asia. This has been called the "Melanesian Continent," because now it has broken up to form the high, but scattered islands of Melanesia. The edge of this continent included Fiji, and may have extended out to parts of Tonga. Its eastern edge is marked on the map. East of this we find two especially deep troughs, known as the Tongan Deep and the Kermadec Deep, with depths of more than 28,000 feet. One place in the Kermadec trough, known as Aldrich Deep, has a sounding of 30,930 feet.
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