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Geology of Cyprus : ウィキペディア英語版 | Geology of Cyprus
The geology of Cyprus is part of the regional geology of Europe. Cyprus lies on the southern border of the Eurasian Plate and on the southern margin of the Anatolian Plate. The southern margin of the Anatolian Plate is in collision with the African Plate, which has created the uplift of the Cyprus arc and Cyprus itself. ==Bedrock geology== Cyprus is commonly divided into four bedrock units,〔(【引用サイトリンク】url=http://www.moa.gov.cy/moa/gsd/gsd.nsf/dmlIntroduction_en/dmlIntroduction_en?OpenDocument# )〕 which are illustrated in the small inset map at the right. From north to south they are: *Keryneia Terrane (blue) *Troodos Ophiolite (red), surrounded by the Circum Troodos Sedimentary Succession (orange) *Mamonia Terrane (green)
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