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| [[Image:Map of Dokdo.png|right|thumb|300px|{{#ifexist:Template:Map of Dokdo.png/credit|{{Map of Dokdo.png/credit}}<br/>|}}Coordinates: 37° 14´ 26.8˝ N, 131° 52´ 10.4˝ E<ref name="koreapdf">[http://www.korea.net/news/issue/attach/45_9095_1_en.pdf Part I: Profile of Dokdo]</ref>]]
| | ''This article is under consideration for '''deletion''' following an author request. The latest version is [https://en.citizendium.org/wiki?title=Dokdo_(Takeshima)&oldid=100724482 here].'' |
| '''Dokdo''' is a small group of volcanic rocks located in the Sea of Japan. South Korea administers the islets as an area of the Ulleung County, Northern Gyeongsang Province. The 56-acre (226600 m<sup>2</sup>) formation consists of two main islands that house a lighthouse, a helicopter pad, and a small police force. Because the rocks shelter various species of birds, plants, and insects, the South Korean government has designated the islets as a nature reserve and enforces measures to protect the islets from the visiting tourists. The sovereignty over Dokdo has been contested by Japan over historical and legal grounds and remains one of the more serious disputes between South Korea and its former colonial ruler. Since at least 1905, the islands were called in Japanese '''Takeshima''' (竹島), meaning the "bamboo island". The Korean name has many different transliterations in English, including "Tok-do", "Dok-to", and "Tok Islets" (<span style="font-family: Batang, Serif">독도</span>), all of which equate to "rocky island". The islets have two English titles: '''Liancourt Rocks''' and '''Hornet Rocks'''. "Liancourt" has its origin in the name of the French whaling ship that first encountered and charted the islets in 1849.
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| == Geography ==
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| [[Image:Dokdo zoomin.png|left|thumb|300px|{{#ifexist:Template:Dokdo zoomin.png/credit|{{Dokdo zoomin.png/credit}}<br/>|}}A detailed map of Dokdo.]]
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| Dokdo lies in the Sea of Japan as a part of an underwater volcano that erupted repeatedly<ref name="cenozoic">{{cite web
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| | title = Geographical and Geological Features of Dokdo
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| | publisher = Truth of Dokdo
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| | url = http://www.truthofdokdo.or.kr/eng/html/story_geography1.html
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| | accessdate = 2007-09-03 }}</ref> from 4.6 to 2.5 million years ago.<ref name="nat">[http://atlas.ngii.go.kr/english/explanation/natural_1_7.jsp Volcanic Landforms], The National Atlas of Korea, retreived 2008-05-10</ref> The underwater Dokdo volcano stands 2 km high on its base with a diameter of 20 ~ 25 km and rises to a guyot<ref name-"adsabs">[http://adsabs.harvard.edu/abs/2007AGUFM.V43D1644K A study on the geophysical characteristics of the summit of the Dokdo volcano in the East Sea (Japan Sea)]</ref> summit that is 10 km wide.<ref name="click">[http://www.clickkorea.org/Dokdo/02.htm History and Culture of Dokdo Islands, Geographical understanding]</ref> The islets on top of this summit consist mostly of trachyte and trachyandesite differentiated from the parental alkali basalt magma of the underwater volcano.<ref name="kang">[http://www.google.com/url?sa=t&ct=res&cd=6&url=http%3A%2F%2Fgeo.khu.ac.kr%2Fmarinesympo%2Ffiles%255C2006Program%26Papers%2F7.Kang.pdf&ei=aC44SOz_DZiQ8wSX8fDYDQ&usg=AFQjCNFr46idnhLHamsB46U15sfcIPQ8pw&sig2=gD3ptoiKZ5LgcoVSoT2Smw Gravity modeling for understanding internal structure of seamounts], Kang Mohee et al, date accessed: 2008-05-24</ref> Samples of these rocks reveal that Dokdo is the oldest existing island in Korea ([[Awaji Island]] is the oldest in Japan)<ref name="oldestjapan">{{cite conference
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| | title = 2003 iEARN Conference News
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| | location = Yumebutai Awaji International Conference site
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| | url = http://www.jearn.jp/2003conference/news/0721.html
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| | accessdate = 2007-09-03 }}</ref>; the second oldest island in Korea is Ulleungdo,<ref name="SNU">{{cite web
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| | title = The Territorial Sovereignty over Dokdo Islets(Liancourt Rocks) and the Cairo Declaration in 1943
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| | publisher = Seoul National University
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| | url = http://plaza.snu.ac.kr/~bigbear1/m3-2-a1.htm
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| | accessdate = 2007-09-03 }}</ref> which formed 2 million years after Dokdo from the same hot spot, with similar igneous composition to Dokdo.<ref name="cenozoic"/> Due to sedimentation, the 2 islands (''Seo-do'' and ''Dong-do'' in Korean, ''Otoko-jima'' and ''Onna-jima'' in Japanese; both literally meaning ''western island'' 西島 and ''eastern island'' 東島, respectively)<ref name="EastWest">{{cite web
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| | title = Special Report: Tokdo-Takeshima Dispute
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| | publisher = Pride of Korea - Dokdo
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| | date = 2001-07-06
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| | url = http://www.google.com/url?sa=t&ct=res&cd=2&url=http%3A%2F%2Fwww.ourdokdo.com%2Freport%2Fdokdo.doc&ei=V3_bRv-7EKXAggSbzInkCQ&usg=AFQjCNHM_57PahcL5TDUy-KdkJf_I06ciQ&sig2=Q4dexuV6Icvowqqp20g3gA
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| | accessdate = 2007-09-02 }}</ref><ref name="mofaname">[http://www.mofa.go.jp/region/asia-paci/takeshima/index.html The Issue of Takeshima], The Ministry of Foreign Affairs of Japan, date accessed: 2008-05-24</ref> that make up most of the island cluster above water split 2 million years ago,<ref name="cenozoic"/> and are now positioned 151 meters apart from each other.<ref name="net">Korea.net (1999–2006). [http://www.korea.net/News/Issues/issueDetailView.asp?board_no=5727 Dokdo: A Profile]. Retrieved [[9 January]], 2006.</ref> The western islet is steeper and larger than the eastern islet, and it is the tallest islet in the cluster.<ref name="corea">[http://www.dokdocorea.com/news-view.htm?p=2&n=5 Dokdocorea.com], date accessed: 2008-05-23</ref> 87 smaller rocks scatter around the two main islands within a radius of a few kilometers,<ref name="ngii">
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| {{cite web
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| | title = Dokdo of Korea
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| | publisher = National Geographic Information Institute
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| | url = http://www.ngii.go.kr/jsp/ngii_eng/html/main/data/data_02.html
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| | accessdate = 2007-09-02 }}</ref> and more than 30 of such geographical features have been named by the South Korean government ministries.<ref name="name">[http://www.dynamickorea.go.kr/news/issues/issueDetailView.asp?board_no=15428&menu_code=A Ten reefs around Dokdo to receive names], Korea.net</ref>
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| == Climate & Ecology ==
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| ==Notes==
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| {{reflist|2}}
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