The Liancourt Rocks are a group of islets in the Sea of Japan between the Korean Peninsula and the Japanese archipelago, made up of two main islets and about 89 smaller rocks covering roughly 19 hectares in total. They formed from volcanic rock erupted in the Cenozoic era, between about 4.6 and 2.5 million years ago, and the western islet reaches the group's highest point at approximately 169 meters. The two main islets, known as the East and West Islet, sit 151 meters apart, about 87 kilometers from South Korea's Ulleungdo and 157 kilometers from Japan's Oki Islands. South Korea administers the islets, though Japan disputes the sovereignty, and a 2006 geological survey found the rocks are eroding quickly. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
Facts
Classification
Protected StatusNational Monument or Landmark 1 Connections
Caused By
Source Liancourt Rocks (Wikipedia)
In Discipline
Wikidata P31 formation-type mapped to discipline Geomorphology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Liancourt Rocks
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Also in Geography Atlas: where this subject is found.
Source Wikidata: Liancourt Rocks
Also in Geography Atlas: where this subject is found.
Source Wikidata: Liancourt Rocks
Sources
1. Liancourt Rocks (Wikipedia)
Lead section
The Liancourt Rocks, known in Korea as Dokdo (Korean: 독도) and in Japan as Takeshima (Japanese: 竹島), are a group of islets in the Sea of Japan between the Korean Peninsula and the Japanese archipelago administered by South Korea.
Article text
The Liancourt Rocks were designated as a breeding ground for band-rumped storm petrels, streaked shearwaters, and black-tailed gulls as Natural Monument #336 of South Korea on November 29, 1982.
View the SourceWikidata: Liancourt Rocks
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