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The South China Sea is a marginal sea that is part of the Pacific Ocean, encompassing an area from the Singapore and Malacca Straits to the Strait of Taiwan of around . The area's importance largely results from one-third of the world's shipping transiting through its waters, and that it is believed to hold huge oil and gas reserves beneath its seabed.
It is located
The minute South China Sea Islands, collectively an archipelago, number in the hundreds. The sea and its mostly uninhabited islands are subject to competing claims of sovereignty by several countries. These claims are also reflected in the variety of names used for the islands and the sea.
The English name is a result of early European interest in the sea as a route from Europe and South Asia to the trading opportunities of China. In the sixteenth century Portuguese sailors called it the China Sea (''Mar da China''); later needs to differentiate it from nearby bodies of water led to calling it the South China Sea. The International Hydrographic Organization refers to the sea as "South China Sea (Nan Hai)".
In Southeast Asia it was once called the ''Champa Sea'' ''Sea of Cham'', after the maritime kingdom of Champa that flourished there before the sixteenth century. The majority of the sea came under Japanese naval control during World War II following the military acquisition of many surrounding South East Asian territories in 1941. Japan calls the sea ''Minami Shina Kai'' "South China Sea". This was written 南支那海 until 2004, when the Japanese Foreign Ministry and other departments switched the spelling 南シナ海, which has become the standard usage in Japan.
In China, it is called the "South Sea", 南海 ''Nánhǎi'', and in Vietnam the "East Sea", ''Biển Đông''. In the Philippines, Malaysia, and Indonesia it was long called the "South China Sea" (''Dagat Timog Tsina'' in Tagalog, ''Laut China Selatan'' in Malay), with the part within Philippine territorial waters often called the "Luzon Sea", ''Dagat Luzon'', by the Philippines. However, following an escalation of the Spratly Islands dispute in 2011, various Philippine government agencies started using the neologism "West Philippine Sea". A Pagasa spokesperson said that the sea to the east of the Philippines will continue to be called the Philippine Sea.
Major rivers that flow into the South China Sea include the Pearl, Min, Jiulong, Red, Mekong, Rajang, Pahang, Pampanga, and Pasig Rivers.
''On the South.'' The Eastern and Southern limits of Singapore and Malacca Straits [A line joining Tanjong Datok, the Southeast point of Johore () through Horsburgh Reef to Pulo Koko, the Northeastern extreme of Bintan Island (). The Northeastern coast of Sumatra] as far West as Tanjong Kedabu () down the East coast of Sumatra to Lucipara Point () thence to Tanjong Nanka, the Southwest extremity of Banka Island, through this island to Tanjong Berikat the Eastern point (), on to Tanjong Djemang () in Billiton, along the North coast of this island to Tanjong Boeroeng Mandi () and thence a line to Tanjong Sambar () the Southwest extreme of Borneo.''On the East.'' From Tanjong Sambar through the West coast of Borneo to Tanjong Sampanmangio, the North point, thence a line to West points of Balabac and Secam Reefs, on to the West point of Bancalan Island and to Cape Buliluyan, the Southwest point of Palawan, through this island to Cabuli Point, the Northern point thereof, thence to the Northwest point of Busuanga and to Cape Calavite in the island of Mindoro, to the Northwest point of Lubang Island and to Point Fuego (14°08'N) in Luzon Island, through this island to Cape Engano, the Northeast point of Luzon, along a line joining this cape with the East point of Balintang Island (20°N) and to the East point of Y'Ami Island (21°05'N) thence to Garan Bi, the Southern point of Taiwan (Formosa), through this island to Santyo (25°N) its North Eastern Point.
''On the North.'' From Fuki Kaku the North point of Formosa to Kiushan Tao (Turnabout Island) on to the South point of Haitan Tao (25°25'N) and thence Westward on the parallel of 25°24' North to the coast of Fukien.
''On the West.'' The Mainland, the Southern limit of the Gulf of Thailand and the East coast of the Malay Peninsula.
The South China Sea opened after around 45 million years ago when the Dangerous Grounds (Reed Tablemount) were rifted away from southern China. Extension culminated in seafloor spreading around 30 million years ago, a process that propagated to the SW resulting in the V-shaped basin we see today. Extension ceased around 17 million years ago. Arguments have continued about the role of tectonic extrusion in forming the basin. Paul Tapponnier and colleagues have argued that as India collides with Asia it pushes Indochina to the SE. The relative shear between Indochina and China caused the South China Sea to open. This view is disputed by geologists who do not consider Indochina to have moved far relative to mainland Asia. Recent marine geophysical studies by Peter Clift has shown that the Red River Fault was active and causing basin formation at least by 37 million years ago in the NW South China Sea, consistent with extrusion playing a part in the formation of the sea. Since opening the South China Sea has been the repository of large sediment volumes delivered by the Mekong River, Red River and Pearl River. Several of these deltas are rich in oil and gas deposits.
The South China Sea contains over 250 small islands, atolls, cays, shoals, reefs, and sandbars, most of which have no indigenous people, many of which are naturally under water at high tide, and some of which are permanently submerged. The features are grouped into three archipelagos (listed by area size), Macclesfield Bank and Scarborough Shoal:
The Spratly Islands spread over an 810 by 900 km area covering some 175 identified insular features, the largest being Taiping Island (Itu Aba) at just over 1.3 km long and with its highest elevation at 3.8 metres.
The largest singular feature in the area of the Spratly Islands is a 100 km wide seamount called Reed Tablemount, also known as Reed Bank, in the northeast of the group, separated from Palawan Island of the Philippines by the Palawan Trench. Now completely submerged, with a depth of 20 m, it was an island until it sank about 7,000 years ago due to the increasing sea level after the last ice age. With an area of 8,866 km², it is one of the largest submerged atoll structures of the world.
The region has proven oil reserves of around 1.2 km³ (7.7 billion barrels), with an estimate of 4.5 km³ (28 billion barrels) in total. Natural gas reserves are estimated to total around 7,500 km³ (266 trillion cubic feet).
According to studies made by the Department of Environment and Natural Resources, Philippines, this body of water holds one third of the entire world's marine biodiversity, thereby making it a very important area for the ecosystem.
China and Vietnam have both been vigorous in prosecuting their claims. The People's Republic of China and South Vietnam each controlled part of the Paracel Islands before 1974. A brief conflict in 1974 resulted in 18 soldiers being killed, and China has controlled the whole of Paracel since then. The Spratly Islands have been the site of a naval clash, in which over seventy Vietnamese sailors were killed just south of Chigua Reef in March 1988. Disputing claimants regularly report clashes between naval vessels.
ASEAN in general, and Malaysia in particular, has been keen to ensure that the territorial disputes within the South China Sea do not escalate into armed conflict. As such, Joint Development Authorities have been set up in areas of overlapping claims to jointly develop the area and dividing the profits equally without settling the issue of sovereignty over the area. This is true, particularly in the Gulf of Thailand. Generally, China has preferred to resolve competing claims bi-laterally, while ASEAN countries prefer multi-lateral talks, believing that they are disadvantaged in bi-lateral negotiations with the much larger China and that because many countries claim the same territory only multilateral talks could effectively resolve the competing claims.
The overlapping claims over Pedra Branca or Pulau Batu Putih including neighboring Middle Rocks by both Singapore and Malaysia were settled in 2008 by the International Court of Justice, awarding Pedra Branca/Pulau Batu Puteh to Singapore and Middle Rocks to Malaysia.
In July 2010, US Secretary of State Hillary Clinton called for the Peoples Republic of China to resolve the territorial dispute. China responded by demanding the US keep out of the issue. This came at a time when both countries have been engaging in naval exercises in a show of force to the opposing side, which increased tensions in the region. The US Military released a statement on August 18 where it opposed the use of force to resolve the dispute, and accused China of assertive behaviour.
Category:Territorial disputes of the Philippines Category:Territorial disputes of the People's Republic of China Category:Territorial disputes of Malaysia Category:Territorial disputes of Vietnam Category:Territorial disputes of the Republic of China Category:Marginal seas of the Pacific Ocean Category:Disputed territories in Southeast Asia
ar:بحر الصين الجنوبي zh-min-nan:Lâm Tiong-kok Hái be:Паўднёва-Кітайскае мора be-x-old:Паўднёва-Кітайскае мора bs:Južno kinesko more br:Mor Su Sina bg:Южнокитайско море ca:Mar de la Xina Meridional cv:Кăнтăр Китай тинĕсĕ cs:Jihočínské moře cbk-zam:Mar de China cy:Môr De Tsieina da:Sydkinesiske Hav de:Südchinesisches Meer et:Lõuna-Hiina meri es:Mar de la China Meridiоnal eo:Sudĉina Maro eu:Hegoaldeko Txinako itsasoa fa:دریای جنوبی چین hif:South China Sea fr:Mer de Chine méridionale fy:Súd-Sineeske See gl:Mar da China Meridional gan:南海 hak:Nàm Chûng-koet Hói ko:남중국해 hi:दक्षिणी चीन सागर hr:Južno kinesko more ilo:Baybay Abagatan a China id:Laut Cina Selatan os:Хуссар Китайы денджыз is:Suður-Kínahaf it:Mar Cinese meridionale he:ים סין הדרומי jv:Segara Cina Kidul pam:Dayat Malat ning Mauling Tsina ka:სამხრეთ ჩინეთის ზღვა kk:Оңтүстік Қытай теңізі sw:Bahari ya Kusini ya China ku:Deryaya Çîna Başûr lv:Dienvidķīnas jūra lt:Pietų Kinijos jūra hu:Dél-kínai-tenger mk:Јужнокинеско Море mr:दक्षिण चीन समुद्र ms:Laut China Selatan mn:Өмнөд Хятадын тэнгис nl:Zuid-Chinese Zee ja:南シナ海 no:Sørkinahavet nn:Sørkinahavet oc:Mar de China Meridionala km:សមុទ្រចិនខាងត្បូង pl:Morze Południowochińskie pt:Mar da China Meridional ro:Marea Chinei de Sud ru:Южно-Китайское море simple:South China Sea sk:Juhočínske more sr:Јужно кинеско море sh:Južno kinesko more su:Laut Cina Kidul fi:Etelä-Kiinan meri sv:Sydkinesiska havet tl:Dagat Luzon ta:தென்சீனக் கடல் th:ทะเลจีนใต้ tr:Güney Çin Denizi uk:Південно-Китайське море ur:بحیرۂ جنوبی چین vi:Biển Đông zh-classical:南海 war:Dagat han Salatan nga Tsina zh-yue:南中國海 zh:南海This text is licensed under the Creative Commons CC-BY-SA License. This text was originally published on Wikipedia and was developed by the Wikipedia community.
| name | Matthew Shaffer |
|---|---|
| birth name | Matthew Joseph Shaffer |
| birth date | May 04, 1978 |
| birth place | Colorado |
| birthname | Matthew Joseph Shaffer }} |
Matthew Joseph Shaffer (born May 4, 1978) is an American musical theatre, television, and film actor, director, executive producer and choreographer. He was born in Florence, Colorado, USA.
This text is licensed under the Creative Commons CC-BY-SA License. This text was originally published on Wikipedia and was developed by the Wikipedia community.
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