翻訳と辞書
Words near each other
・ Prehistory of association football
・ Prehistory of Australia
・ Prehistory of Brittany
・ Prehistory of Colorado
・ Prehistory of Corsica
・ Prehistory of France
・ Prehistory of Iran
・ Prehistory of Laguna (province)
・ Prehistory of Manila
・ Prehistory of Marinduque
・ Prehistory of Myanmar
・ Prehistory of Northern Nigeria
・ Prehistory of Pampanga
・ Prehistory of Sarangani
・ Prehistory of Sri Lanka
Prehistory of Taiwan
・ Prehistory of the Armenians
・ Prehistory of the Balkans
・ Prehistory of the Levant
・ Prehistory of the Philippines
・ Prehistory of the United States
・ Prehistory of the Valencian Community
・ Prehistory of Transylvania
・ Prehistory of West Virginia
・ Prehistory to 1st century BC in Canada
・ Prehn Peninsula
・ Prehn's sign
・ Prehnite
・ Prehnite-pumpellyite facies
・ Prehomogeneous vector space


Dictionary Lists
翻訳と辞書 辞書検索 [ 開発暫定版 ]
スポンサード リンク

Prehistory of Taiwan : ウィキペディア英語版
Prehistory of Taiwan

The prehistory of Taiwan, ending with the arrival of the Dutch East India Company in 1624, is known from archaeological finds throughout the island. The earliest evidence of human habitation dates back 20,000 to 30,000 years, when the Taiwan Strait was exposed by lower sea levels as a land bridge. Around 5,000 years ago farmers from the southeast Chinese coast settled on the island. These people are believed to have been speakers of Austronesian languages, which dispersed from Taiwan across the islands of the Pacific and Indian Oceans. The current Taiwanese aborigines are believed to be their descendants.
== Geographical context ==
(詳細はconvergent boundary between the continental Eurasian Plate and the oceanic Philippine Sea Plate. The boundary continues southwards in the Luzon Volcanic Arc, a chain of islands between Taiwan and the Philippine island of Luzon including Green Island and Orchid Island. From the northern part of the island the eastward continuation of the boundary is marked by the Ryukyu chain of volcanic islands.〔(【引用サイトリンク】url=http://twgeog.geo.ntnu.edu.tw/english/geology/geology.htm )〕〔(【引用サイトリンク】title=Geology of Taiwan )
The island is separated from the coast of Fujian to the west by the Taiwan Strait, which is 130 km wide at its narrowest point. The most significant islands in the Strait are the Penghu islands 45 km from the southwest coast of Taiwan and 140 km from the mainland. Part of the continental shelf, the Strait is no more than 100 m deep, and has become a land bridge during glacial periods.
Taiwan is a tilted fault block, with rugged longitudinal mountain ranges making up most of the eastern two-thirds of the island. They include more than two hundred peaks with elevations of over 3,000 m (9,843 ft). The western side of the island slopes down to fertile coastal plains. The island straddles the Tropic of Cancer, and has a humid subtropical climate.
The original vegetation ranged from tropical rainforest in the lowlands through temperate forests, boreal forest and alpine plants with increasing altitude.

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
ウィキペディアで「Prehistory of Taiwan」の詳細全文を読む



スポンサード リンク
翻訳と辞書 : 翻訳のためのインターネットリソース

Copyright(C) kotoba.ne.jp 1997-2016. All Rights Reserved.