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The island of Taiwan was formed approximately 4 to 5 million years ago at a convergent boundary between the Philippine Sea Plate and the Eurasian Plate. In a boundary running the length of the island and continuing southwards, the Eurasian Plate is sliding under the Philippine Sea Plate. In the northeast of the island, the Philippine Sea Plate slides under the Eurasian Plate.Most of the island comprises a huge fault block tilted to the west.

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  • Geology of Taiwan (en)
  • 台灣地質 (zh)
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  • 臺灣位於菲律賓海板塊和歐亞板塊的聚合邊界,為一個造山作用活躍的活動構造區,根據GPS觀測資料,菲律賓海板塊以每年8.2公分的移動速度向西北移動。菲律賓海板塊的隱沒方向在臺灣南方,歐亞板塊朝東隱沒到菲律賓海板塊之下,形成馬尼拉海溝及其東側的,到了臺灣北方,菲律賓海板塊則是朝北隱沒到歐亞板塊之下,造成琉球海溝及其北側的和沖繩海槽。 (zh)
  • The island of Taiwan was formed approximately 4 to 5 million years ago at a convergent boundary between the Philippine Sea Plate and the Eurasian Plate. In a boundary running the length of the island and continuing southwards, the Eurasian Plate is sliding under the Philippine Sea Plate. In the northeast of the island, the Philippine Sea Plate slides under the Eurasian Plate.Most of the island comprises a huge fault block tilted to the west. (en)
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/Central_Range.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Philippine_Sea_Plate_br.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Beitou_Thermal_Valley_warning_sign_20050814.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Haian_Range,_Taiwan.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Taiwan_seismicity.jpg
  • http://commons.wikimedia.org/wiki/Special:FilePath/Taiwan_tectonics_block_diagram.png
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