Pacific Documentation - Lost World of The Pacific - Polynesian Islands Documentary
Pacific Documentation -
Lost World of
The Pacific - Polynesian
Islands Documentary
Polynesia is characterized by a small amount of land spread over a very large portion of the mid and southern
Pacific Ocean. Most
Polynesian islands and archipelagos, including the
Hawaiian Islands and
Samoa, are composed of volcanic islands built by hotspots.
New Zealand,
Norfolk Island, and
Ouvéa, the
Polynesian outlier near
New Caledonia, are the unsubmerged portions of the largely sunken continent of
Zealandia. Zealandia is believed to have mostly sunk by 23 m.y.a. and resurfaced geologically recently due to a change in the movements of the
Pacific Plate in relation to the
Indo-Australian plate, which served to uplift the New Zealand portion. At first, the
Pacific plate was subducted under
the Australian plate. The Alpine Fault that traverses the
South Island is currently a transform fault while the convergent plate boundary from the
North Island northwards is a subduction zone called the
Kermadec-Tonga Subduction Zone. The volcanism associated with this subduction zone is the origin of the Kermadec and
Tongan island archipelagos.
Out of about
117,
000 or
118,000 square miles (
300,000 or
310,000 km2) of land, over 103,000 square miles (270,000 km2) are within New Zealand; the
Hawaiian archipelago comprises about half the remainder. The Zealandia continent has approximately 1,400,000 square miles (3,600,000 km2) of continental shelf. The oldest rocks in the region are found in New Zealand and are believed to be about 510 million years old. The oldest Polynesian rocks outside of Zealandia are to be found in the
Hawaiian Emperor Seamount Chain, and are 80 million years old.
Geographic area
Polynesia is generally defined as the islands within the
Polynesian Triangle, although there are some islands that are inhabited by
Polynesian people situated outside the Polynesian Triangle. Geographically, the Polynesian Triangle is drawn by connecting the points of
Hawaii, New Zealand and
Easter Island.
The other main island groups located within the Polynesian Triangle are Samoa,
Tonga, the
Cook Islands,
Tuvalu,
Tokelau,
Niue,
Wallis and Futuna and
French Polynesia.
There are also small Polynesian settlements in
Papua New Guinea, the
Solomon Islands, the
Caroline Islands, and in
Vanuatu. An island group with strong Polynesian cultural traits outside of this great triangle is
Rotuma, situated north of
Fiji.
The people of Rotuma have many common Polynesian traits but speak a non-Polynesian language. Some of the
Lau Islands to the southeast of Fiji have strong historic and cultural links with Tonga.
However, in essence, Polynesia is a cultural term referring to one of the three parts of
Oceania (the others being
Micronesia and Melanesia).
DNA studies suggest that the indigenous
Pacific Islands population migrated from
Taiwan thousands of years ago and dispersed throughout the region into three distinct cultural groups.
Island groups
Mokoliʻi
Isle near
Oahu, Hawaii
Cook's Bay on Moorea, French Polynesia
The following are the islands and island groups, either nations or overseas territories of former colonial powers, that are of native
Polynesian culture or where archaeological evidence indicates Polynesian settlement in the past.[3] Some islands of Polynesian origin are outside the general triangle that geographically defines the region.
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Don´t miss: "
Cute Monkey -
Funny Monkies -
Compilation"
➨ https://www.youtube.com/watch?v=YhvP-zw1k-I
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Please watch: "Pacific Documentation - Lost World of The Pacific - Polynesian Islands Documentary"
➨ https://www.youtube.com/watch?v=OPbrv84yzFg