The Gulf of Thailand (or Gulf of Siam) is a gulf that borders, but is not part of the South China Sea (Pacific Ocean). The gulf is bordered by Cambodia, Thailand and Vietnam. The northern tip of the gulf is the Bay of Bangkok at the mouth of the Chao Phraya River, near Bangkok. The gulf covers roughly 320,000 km². The boundary of the gulf is defined by the line from Cape Bai Bung in southern Vietnam (just south of the mouth of the Mekong river) to the city Kota Baru on the Malayian coast. At the height of the last ice age the Gulf of Thailand did not exist, due to the lower sea level, the location being part of the Chao Phraya river valley.
Geography
The gulf is relatively shallow: the mean depth is 45
m, and the maximum depth only 80 m. This makes water exchange slow, and the strong water inflow from the rivers make the Gulf low in
salinity (3.05-3.25%) and rich in
sediments. Only at the greater depths does water with a higher salinity (3.4%) flow into the gulf from the
South China sea and fills the central depression below a depth of 50 m. The main rivers which empty into the gulf are the Chao Phraya (including its distributary
Tha Chin River),
Mae Klong and
Bang Pa Kong Rivers at the
Bay of Bangkok, and to a lesser degree the
Tapi River into
Bandon Bay in the southwest of the gulf.
Due to the tropical warmth of the water, the Gulf of Thailand harbours many coral reefs, and thus several diving resorts. Most popular for tourism is the island Ko Samui in the Surat Thani province, Pattaya Chonburi province, while Ko Tao is the center of the diving tourism.
Natural resources
The gulf also contains some
oil and larger
natural gas resources in Thai and Cambodian territorial water.
Dispute
There is a territorial dispute in the area between Malaysia, Thailand and Vietnam. Malaysia and Thailand in particular have chosen to jointly develop the disputed areas.