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Liancourt Rocks

Group of disputed islets in the Sea of Japan

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Liancourt rocks, in Japan called Takeshima and in North and South Korea called Dokdo (Tokto).
demis.nl · Public domain

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South Korea exercises sovereignty over the islets, while Japan claims sovereignty over them. South Korean government's stated position is that the islets are integral part of Korean territory historically, geographically and under international law, that no territorial dispute exists over them, and that they are therefore not a matter to be dealt with through diplomatic negotiation or judicial settlement. North Korea formerly claimed the territory, but has reportedly ceased its claim, following the country's abandoning of all goals of reunification with the South. South Korea classifies the islets as Dokdo-ri, Ulleung-eup, Ulleung County, North Gyeongsang Province, while Japan classifies the islands as part of Okinoshima, Oki District, Shimane Prefecture.

Geography

The Liancourt Rocks consist of two main islets and numerous surrounding rocks. The two main islets, called Seodo (서도; 西島; lit. 'western island') and Dongdo (동도; 東島; lit. 'eastern island') in Korean and Ojima (男島; "Male Island") and Mejima (女島; "Female Island") in Japanese, are 151 metres (495 ft) apart. The Western Island is the larger of the two, with a wider base and higher peak, while the Eastern Island offers more usable surface area.

Altogether, there are about 90 islets and reefs, volcanic rocks formed in the Cenozoic era, more specifically 4.6 to 2.5 million years ago. A total of 37 of these islets are recognized as permanent land.

The total area of the islets is about 187,554 square metres (46.346 acres), with their highest point at 168.5 metres (553 ft) on the West Islet. The western islet is about 88,740 square metres (21.93 acres); the eastern islet is about 73,300 square metres (18.1 acres). The western islet consists of a single peak and features many caves along the coastline. The cliffs of the eastern islet are about 10 to 20 metres (33 to 66 ft) high. There are two large caves giving access to the sea, as well as a crater.

In 2006, a geologist reported that the islets formed 4.5 million years ago and are (in a geological sense) quickly eroding.

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