Gulf of Thailand
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Gulf of Thailand
Gulf of Thailand
Gulf of Siam
Gulf of Thailand.svg
Location of the gulf
Location Southeast Asia
Coordinates 09°30?N 102°00?E / 9.500°N 102.000°E / 9.500; 102.000Coordinates: 09°30?N 102°00?E / 9.500°N 102.000°E / 9.500; 102.000
Type Gulf
Primary inflows South China Sea
Surface area 320,000 km2 (120,000 sq mi)
Average depth 58 m (190 ft)
Max. depth 85 m (279 ft)

The Gulf of Thailand, formerly the Gulf of Siam, is a shallow inlet[1][2] in the western part of the South China and Eastern Archipelagic Seas, a marginal body of water in the western Pacific Ocean. The gulf is around 800 km (497 mi) long and up to 560 km (348 mi) wide, has a surface area of 320,000 km2 (123,553 sq mi) and is surrounded on the north, west and southwest by Thailand, on the northeast by Cambodia and Vietnam. The South China Sea is to the southeast.[3][4]


The modern Thai name of the gulf is Ao Thai (Thai: ?,  [?à:w tj], "Thai Gulf") and "Gulf of Thailand" has been adopted as the official name of the body by the International Hydrographic Organization.[5][when?] Its name in Malay and Khmer continues to be the "Gulf of Siam", Teluk Siam and Khmer: , Chhoung Samut Siem, respectively. In Thai, the gulf is historically known as Ao Sayam (Thai: ).[6] In Vietnamese it is known as V?nh Thái Lan.

It is generally identified with the Great Gulf (Latin: Magnus Sinus) known to Greek, Roman, Arab, Persian, and Renaissance cartographers before the influx of Portuguese explorers removed the phantom Dragon Tail peninsula from European world maps in the 16th century.


Map showing the location of the gulf

The Gulf of Thailand is bordered by Cambodia, Thailand, and Vietnam. It occupies a seabed area of 304,000 km2 from 6° N to 13°30' N latitude and 99°E to 104° E longitude.[7]:250 The northern tip of the gulf is the Bay of Bangkok at the mouth of the Chao Phraya River. The southern boundary of the gulf is defined by a line from Cape Bai Bung in southern Vietnam (just south of the mouth of the Mekong River) to the city of Kota Bharu on the Malaysian coast.

The gulf is relatively shallow: its mean depth is 58 metres (190 ft) and the maximum depth is only 85 metres (279 ft).[7]:250 This makes water exchange slow, and the strong water inflow from the rivers reduce the level of salinity in the gulf (3.05-3.25 percent) and enriches the sediments. Only at greater depths does water with a higher salinity (3.4 percent) flow into the gulf from the South China Sea. It fills the central depression below a depth of 50 metres (160 ft). The main rivers which empty into the gulf are the Chao Phraya, including its distributary Tha Chin River, the Mae Klong, and Bang Pakong rivers at the Bay of Bangkok, and to a lesser degree the Tapi River flowing into Bandon Bay in the southwest of the gulf.

The International Hydrographic Organization defines the southern limit of the gulf as "[a] line running from the Western extreme of Cambodia or Camau Point (8°36'N) to the Northern extreme of the point on the East side of the estuary of the Kelantan River (6°14?N 102°15?E / 6.233°N 102.250°E / 6.233; 102.250)".[5]

Seabed morphology

The seabed morphology in the central depression of the gulf is characterised by the presence of elongated mounds and ridges arranged parallel to the axis of the basin. This morphology, widespread within the gulf in water depths exceeding 50 m, covers an area of tens of thousands of square kilometres.

It reflects an interaction between sediment dewatering and the erosional activity of the present-day bottom currents.[8] The sediment dewatering and fluid seepage result in the formation of numerous small pits and pockmarks. The long-term erosion imposed by currents of stable orientation modifies pockmarks into long runnels and depressions, and ultimately leads to the formation of the large fields of elongated mounds and ridges, as well as the residual outliers of un-eroded mud and clay sheets.[8]


  • Vinh Tuan Ven
  • Vinh Ba Hon
  • Vinh Hon Chong


The larger islands in the gulf include:


Coral reefs

There are 75,590 rai of coral reef in the gulf, of which five percent are considered to be in fertile condition. In 2010 severe coral bleaching occurred at most reef sites in the country. Bleaching of reefs in the Andaman Sea was more severe and extensive than that in the Gulf of Thailand.[9] In 2016, coral bleaching was detected at Ko Thalu and Ko Lueam in Prachuap Khiri Khan Province for the first time.[10]

Water quality

Coastal water monitoring results in 2015 from 202 sampling locations, collected twice annually, indicate that no Thai coastal waters were found to be in excellent condition. Sixteen percent of coastal water was of good quality, 72 percent was of fair quality, 9 percent was of poor quality and 3 percent was of very poor quality. The quality of all coastal waters exhibited similar percentages -- most were of fair quality -- except for the Inner Gulf of Thailand, where the coastal water was poor to very poor. In comparison to coastal water quality as measured in 2014, water quality has deteriorated.[11]:52 Some gulf waters off Chachoengsao Province, Samut Sakhon Province, Samut Prakan Province, Bangkok, Rayong Province, Chonburi Province, Phetchaburi Province, Prachuap Khiri Khan Province, and Surat Thani Province were judged to have coastal waters in "poor" or "very poor" condition.[11]:54Songkhla was the only province on the gulf with coastal water rated "good" quality.[11]:56


Of Thailand's total marine catch, 41 percent is caught in the Gulf of Thailand and 19 percent in the Andaman Sea. Forty percent is caught in waters outside Thailand's EEZ.[9]

Coastal erosion

Thailand has 1,660 kilometres of coastline bordering the gulf. "Severe erosion", more than five metres of coastline loss per year, afflicts 670 kilometres of that total. At least some of the erosion is attributable to the clearing of mangrove forests to make way for shrimp farms.[12]


Eden's whale feeds in the gulf
Eden's whale off Bang Tapun.

The gulf's many coral reefs have made it attractive to divers. The tropical warmth of the water attracts many tourists. Some of the most important tourist destinations in the Gulf of Thailand are the islands of Ko Samui and Ko Pha Ngan in Surat Thani Province, Pattaya in Chonburi Province, Cha-am in Phetchaburi Province, Hua Hin in Prachuap Khiri Khan Province, and Ko Samet in Rayong Province.

In recent years, the bay has become known for its whale watching activities, targeting the endemic, critically endangered populations of cetaceans (Eden's whales, newly described Omura's whales,[]Chinese white dolphins, and Irrawaddy dolphins showing unique feeding behaviors), and dugongs.[13][14][15] It was first classified by Müller in 1776 as Trichechus dugon.[16] Presence of a critically endangered Hawksbill sea turtle, a rare species in Thai waters, was confirmed during whale watching expeditions in January, 2016.[17]

Territorial disputes

The area between Malaysia, Thailand, Cambodia, and Vietnam is subject to several territorial disputes. Malaysia and Thailand have chosen to jointly develop the disputed areas, which include the islands of Ko Kra and Ko Losin.[18] A long-standing dispute between Cambodia and Vietnam in the Gulf of Thailand concerns mainly the island of Phú Qu?c or Koh Tral in Khmer, which is off the Cambodian coast.[19] Cambodia also claims 48,000 square kilometres (19,000 sq mi) of shelf area.[20][21]

See also


  1. ^ "Marine Gazetteer browser". Marineregions org. Retrieved 2016. 
  2. ^ "Thailand, Gulf of". Oxford University Press. Retrieved 2016. 
  3. ^ "Marine Gazetteer Placedetails - Gulf of Thailand". Marineregions org. Retrieved 2016. 
  4. ^ "Gulf of Thailand". Retrieved 2016. 
  5. ^ a b "Limits of Oceans and Seas" (PDF) (3 ed.). International Hydrographic Organization. 1953. p. 23. Retrieved 2010. 
  6. ^ ? ?.?. 2470 [A report on the royal travel through the Gulf of Siam, 1927] (pdf). Royal Thai Government Gazette (in Thai). Bangkok: Cabinet Secretariat. 88 (D): 44. 1927-05-22. Retrieved . 
  7. ^ a b Khongchai, Narongsak; Vibunpant, Somchai; Eiamsa-ard, Monton; Supongpan, Mala. "Preliminary Analysis of Demersal Fish Assemblages in Coastal Waters of the Gulf of Thailand" (PDF). Worldfish. Archived from the original (PDF) on 19 February 2015. Retrieved 2015. 
  8. ^ a b Puchala, R. (2014), Morphology and origin of modern seabed features in the central basin of the Gulf of Thailand, doi:10.13140/RG.2.1.3891.0808 (inactive 2017-01-19) 
  9. ^ a b Oceans in the Balance, Thailand in Focus (PDF). Bangkok: Greenpeace Southeast Asia (Thailand). c. 2012. Retrieved 2017. 
  10. ^ Wipatayotin, Apinya (2016-04-04). "Rising sea temps bring coral bleaching to Gulf". Bangkok Post. Retrieved 2016. 
  11. ^ a b c Thailand State of Pollution Report 2015 (PDF). Bangkok: Pollution Control Department, Ministry of Natural Resources and Environment (Thailand). 2016. ISBN 978-616-316-327-1. Retrieved 2017. 
  12. ^ Wipatayotin, Apinya (10 December 2017). "Shoring up defences". Bangkok Post Spectrum. 10 (50). Retrieved 2017. 
  13. ^ "Dugongs and seagrass in Thailand: Present status and future challenges" (PDF). Phuket Marine Biological Center and Department of Marine and Coastal Resources. pp. 41-50. Retrieved 2016. 
  14. ^ "Conservation of the Dugong (Dugong Dugon) on the Eastern Coast of the Gulf of Thailand" (PDF). Ocean Park Conservation Foundation Aberdeen, Hong Kong & Project Aware, Australia. May 1, 2004. Retrieved 2016. 
  15. ^ Marsh, H. et al. (2002). Dugong: status reports and action plans for countries and territories Archived 2007-05-08 at the Wayback Machine.. IUCN.
  16. ^ Dugong dugon. The Paleobiology Database. Retrieved on 22 July 2007.
  17. ^
  18. ^ "Defining areas for joint development in disputed waters - Malaysia-Thailand p. 13". University of Wollongong. Retrieved 2016. 
  19. ^ Prescott, J. R. V. (1978). Boundaries and Frontiers. Rowman and Littlefield. ISBN 0847660869. 
  20. ^ Paul Ganster & David E. Lorey, Borders and border politics in a globalizing world.
  21. ^ Schofield, Clive (2008). "Maritime Claims, Conflicts and Cooperation in the Gulf of Thailand". Ocean Yearbook Online. Koninklijke Brill NV. 22: 75. doi:10.1163/221160008x00064. Retrieved 2016. 

External links

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