|Native name: 沖ノ鳥島, Okinotori-shima|
|Location||Philippine Sea, Pacific Ocean|
|Total islands||1 atoll with 2 islets|
|Area||7.8 km2 (3.0 sq mi)|
|Highest elevation||1.5 m (4.9 ft)|
|Highest point||unnamed point|
The Okinotori Islands (沖ノ鳥島 Okinotori-shima?) "distant bird island" are an 8 km2 total area uninhabited atoll. Its dry land area however is mostly made up by 3 concrete encasings amounting to over 8000 m2; it furthermore has a 5000 m2 platform in its lagoon housing a research station.
It is located on the Palau-Kyushu Ridge in the Philippine Sea at Coordinates: , 534 km (332 mi) SE of Oki Daitō and 567 km (352 mi) WSW of Minami Iwo Jima of the Ogasawara Islands or 1,740 km (1,080 mi) south of Tokyo, Japan. The Japanese meaning of the name is "remote bird islands" and they are sometimes referred to as "the southernmost islands of Japan".
The atoll has multiple designations in English (Okinotori coral reefs, Okinotori Islands). Its original name was Parece Vela, Spanish for "looks like a sail" (alluding to the original appearance of the reef). This name has been retained in English as well, especially to designate the geological formations of the islets.
It was possibly first sighted by the Spanish sailor Bernardo de la Torre in 1543, certainly by Miguel López de Legazpi in 1565, and its first recorded name was Parece Vela ("looks like a sail" in Spanish).
In 1789, William Douglas arrived with British ship Iphigenia and, in the following year, the place was named Douglas Reef (also spelt Douglass Reef). The existence of the atoll might not have been known by the Japanese until 1888. In 1922 and 1925, the Japanese navy ship Manshu[disambiguation needed] investigated the area. In 1931, confirming that no other countries had claimed the reefs, Japan declared it Japanese territory, placing it under the jurisdiction of the Tokyo Metropolis, classifying it as part of the Ogasawara Village, and naming it Okinotorishima.
During 1939 and 1941 a foundation was completed for "a lighthouse and a meteorological observation site"; however, construction was interrupted by the outbreak of World War II. After Japan's defeat, the United States assumed sovereignty over the Ogasawara islands, and returned authority over the islands to Japan in 1968.
Between 1987 and 1993 the government of Tokyo and later the central government built steel breakwaters and concrete walls, to stop the erosion of Okinotorishima, which today leaves only three of the five rocks that were present in 1939 above water; in 1988 the Japan Marine Science and Technology Center built a marine investigation facility which it has since maintained following typhoon damage.
Geologically, the islets are an atoll, built on the Kyushu-Palau Ridge, the westernmost part of the Izu-Bonin-Mariana Arc System. The name "Parece Vela" has been given to the extinct back-arc basin that lies immediately to the east (the northern half of this back-arc basin is known as the Shikoku Basin). This back-arc basin formed by seafloor spreading between late Oligocene and Miocene. The Parece Vela Basin contains the longest megamullion in the world. The original Spanish name of the islets is normally used for the geological formations, hence, Parece Vela megamullion, Parece Vela ridge, Parece Vela rift or Parece Vela basin.
The waters around the reefs are potentially rich in oil and other resources and it lies in an area of potential military significance. At high tide, one area of the reefs is roughly the size of a twin bed and pokes just 7.4 centimeters (2.9 inches) out of the ocean. The other is the size of a small bedroom and rises about twice as high. The entire reef consists of approximately 7.8 square kilometers (3.0 sq mi), most of which is submerged even at low tide.
The area has three tiny individual islets:
- Higashi-Kojima (東小島, "Eastern Islet")
- Kita-Kojima (北小島, "Northern Islet"), nevertheless rather in the West
- Minami-Kojima (南小島, "Southern Islet")
Minami-Kojima is a completely artificial islet created in shallow water. But also the two original islets appear completely artificial today, with little if any trace of the two natural rocks that still appear on photographs of 1987. In 1925, there were still five above-water rocks, which have eroded since. A report from 1947 mentions five above-water rocks. Three smaller ones were on the west side, nearly impossible to see from seaward because of the breaking waves. The larger rocks on the southwest side and on the northeast side, possibly Kita-Kojima and Higashi-Kojima, were reported to be 0.6 m (2 ft) and 0.4 m (16 inches) high, respectively. The original rocks appeared barren, obviously without any terrestrial vegetation. The current artificial dry land areas with their concrete surfaces appear unfit to support terrestrial vegetation either.
After concrete encasing, each of the islets appears as a circle with a diameter of 60 meters (about 200 ft) on detailed satellite images, which would correspond to a land area—albeit mostly artificial—of 2827 m2 (0.7 acres) per islet, or 8482 m2 (2.1 acres) in total. In addition, there is a platform on stilts in the shallow part of the lagoon 140 meters (460 ft) ENE of the southern islet, built by the Japan Marine Science and Technology Center in 1988, which appears as a rectangle of 100 m by 50 m (330 ft by 165 ft). The platform has a helicopter landing pad and a large three-story building with a marine investigation facility and a meteorological station.
The rocks are in the western part of a lagoon surrounded by a submerged coral reef, over which the waves break, and that extends 4.5 km (2.8 mi) east-west and 1.7 km (1.1 mi) north-south, with an area of roughly 5 km² within the rim of the reef. The lagoon is 3 to 4.6 meters deep, but there are numerous coral heads of lesser depths throughout the area. The fringing reef of the atoll is pear-shaped in an east-west direction with its greatest width at the eastern end. There is a small boat channel into the lagoon in the southwest, about 15 meters (50 ft) wide and 6 meters (20 ft) deep, 250 meters (800 ft) southeast of the artificial islet.
Administratively, the island is considered part of Ogasawara village, Tokyo. In 1939, the construction of a Naval Base was started by Japan, but suspended in 1941, at the start of the World War II hostilities in the Pacific.
In order to prevent the island from submersion caused by erosion and maintain the claim to the EEZ, the Japanese government launched an embankment building project in 1987, and Higashikojima and Kitakojima were surrounded by concrete. Japan has encased the reefs with $280 million worth of concrete and covered the smaller one with a $50 million titanium net to shield it from debris thrown up by the ocean's waves. In fact, the Japanese government has spent over $600 million fortifying the reefs to prevent them from being completely washed away.
Furthermore, the Nippon Foundation has drawn plans to build a lighthouse and increase the size of the reef by breeding microorganisms known as foraminifera. Creating land using the microorganisms could take decades to a century before the island is large enough to be useful.
In 2005, the government installed a radar system (at the cost of ¥ 330 million), repaired a heliport, and placed an official address plaque saying, "1 Okinotori Island, Ogasawara Village, Tokyo" in Japanese. Fishing expeditions are also sent to support the claim of economic activity.
Tokyo Governor Shintaro Ishihara has talked of building a power station, despite protests by environmentalists. His government has helped fund expeditions to Okinotori by Japanese fishermen and scientists. Governor Ishihara himself toured the islands on May 20, 2005 to inspect the conservation and management efforts, went snorkeling to see firsthand the condition of the surrounding waters, and released Japanese horse mackerel fry to show support for the local fishing industry. The islands are an intermittent rallying point for Japanese nationalists, and, as such, a hot-button political issue in Japan.
On 22 April 2004, Chinese diplomats stated during bilateral talks with Japan that they regarded Okinotorishima as an atoll, not an islet, and did not acknowledge Japan's claim to an exclusive economic zone (EEZ) stemming from Okinotorishima.
Under the United Nations Convention on the Law of the Sea, an island is "a naturally formed area of land, surrounded by water, which is above water at high tide". It states that "rocks which cannot sustain human habitation or economic life of their own shall have no exclusive economic zone." Japan signed the Convention in 1983; the Convention came into force in 1994–1996 for Japan.
Japan claims an EEZ over 400,000 square km (154,500 square miles) around Okinotorishima. The People's Republic of China disputes this claim, saying the area only consists of rocks and not islands. The PRC has not made a territorial claim of its own regarding Okinotorishima, but foreign policy analysts note that it wants to "investigate the surrounding seabed for submarine operations in case of military conflict involving the Republic of China (Taiwan)."
The territory lies at a militarily strategic point, midway between Taiwan and Guam, the latter where U.S. forces are based. Vessels of the PRC are believed to have been mapping the ocean's bottom over which U.S. warships might pass on their way to Taiwan. The PRC conducted four maritime surveys near the Okinotori coral reefs in 2001, two in 2002, and one in 2003. However, the number of such incidents rose to four in 2004. These incidents have drawn protests from Japan.
Jon Van Dyke, a law professor, has suggested that the situation is similar to the failed British attempt to claim an EEZ around Rockall, an uninhabited granite outcropping in the Atlantic Ocean. The UK eventually dropped its claim in the 1990s when other countries objected. Dr. Dyke has further asserted that it is impossible to make "a plausible claim that Okinotorishima should be able to generate a 200 [nautical]-mile zone". Tadao Kuribayashi, another law professor, disagrees, arguing in part that rocks and reefs differ in composition and structure, and that the intent of the provision was geared toward the former.
- Foreign relations of Japan: Disputed territories
- Scarborough Shoal
- Japanese nationalism
- Chinese nationalism
- Extreme points of Japan
- Johnson South Reef—EEZ Dispute
- Macclesfield Bank
- Yukie Yoshikawa. 2005. "Okinotorishima: Just the Tip of the Iceberg". Harvard Asian Quarterly, Vol. 9, No. 4.
- Viajeros Celtíberos ignorados, archived from the original on 17 Sep 2010, retrieved 11 May 2012
- Oceanic core complexes along the Parece Vela Rift, archived from the original on 20 February 2012, retrieved May 4, 2012
- "Anomalous Topography in the Parece Vela Basin.", Report of Hydrographic Researches, 37, 2001: 9–18, retrieved 4 May 2012
- Salisbury, Matthew H., Gigamullion Drilling in the Philippine Sea, retrieved 6 May 2012
- Ohara, Yasuhiko; Fujioka, Kantaro; Teruaki, Ishii; Yurimoto, Yurimoto (2003), "Peridotites and gabbros from the Parece Vela backarc basin: Unique tectonic window in an extinct backarc spreading ridge", Geochemistry Geophysics Geosystems 4 (4): 8611, retrieved 6 May 2012
- Onishi, Norimitsu. "Japan and China Dispute a Pacific Islet," New York Times. July 10, 2005.
- Martin Fackler. 2005, February 16. "A Reef or a Rock? Question Puts Japan In a Hard Place To Claim Disputed Waters, Charity Tries to Find Use For Okinotori Shima" Wall Street Journal. p. A1.
- Martin Fackler. 2005, February 20. "Japan's ultranationalists: Stuck between a rock and a hard sell"
- Xinhua. 2005, August 25. "Japan hopes to build lighthouse on atoll disputed with China."
- Campion, Gilles, (AFP-JiJi), "Remote rocks at center of dispute", Japan Times, March 13, 2010, p. 3.
- Yukie YOSHIKAWA. 2007, October 11. "The US-Japan-China Mistrust Spiral and Okinotorishima"
|Wikimedia Commons has media related to Okinotorishima.|
- Page with overhead photograph of the entire atoll
- report about appearance in 1947 (under the name Parece Vela/Douglas Reef)
- close-up photo of Higashikojima (東小島, "Eastern Islet")
- page with photograph of platform
- Italian page with history in English and oblique aerial photograph of Okinotori from southwest
- detailed satellite images
- Japanese map
- Tokyo governor stirs reef dispute