The Mekong Delta ( or simply ), also known as the South-western Region () or the Western Region (), is the region in southwestern Vietnam where the Mekong River delta through a network of distributary. The Mekong delta region encompasses a large portion of south-western Vietnam, of an area of over . Mekong Delta () on ARCBC (ASEAN Regional Centre for Biodiversity Conservation) site The size of the area covered by water depends on the season. Its wet coastal geography makes it an important source of agriculture and aquaculture for the country.
The delta has been occupied as early as the 4th century BC. As a product of Khmer people, Vietnamese, Chinese, and French settlement in the region, the delta and its waterways have numerous names, including the Khmer language term Bassac River to refer to the lower basin and the largest river branch flowing through it. After the 1954 Geneva Conference, Vietnam was split into two with South Vietnam inheriting the southern half of Vietnam becoming the State of Vietnam and eventually the South Vietnam, also known as South Vietnam, with their own administrative states (see Provinces of South Vietnam). After 1975, the Mekong Delta ceased being a part of the Republic of Vietnam, succeeded by the current Vietnamese nation. The region comprises 4 provinces: Đồng Tháp, An Giang, Vĩnh Long, and Cà Mau, along with the province-level municipality of Cần Thơ.
The Mekong Delta has been dubbed a "biological treasure trove". Over 1,000 animal species were recorded between 1997 and 2007 and new species of plants, fish, lizards, and mammals have been discovered in previously unexplored areas, including the Laotian rock rat, thought to be extinct. The low-lying coastal geography of the region makes it vulnerable to climate change caused sea level rise, alongside related issues such as coastal erosion and saltwater intrusion.
Angkor Borei is a site in the Mekong Delta that existed between 400 BC-500 AD. This site had extensive maritime trade networks throughout Southeast Asia and with India, and is believed to have possibly been the ancient capital to the civilization of Funan.
In 1658, without any excuses, the Nguyễn invaded Cambodia and deposed the only Khmer Muslim king Ramathipadi I (Sultan Ibrahim). 16 years later, the Nguyễn again militarily interfered Cambodian internal royal affairs, putting Prince Ang Nan into power. The Nguyễn invited fleeing Chinese refugees to settle in Mekong River entrance towns of Mỹ Tho and Biên Hoà In 1688, the Chinese revolted against Nguyễn lords. King Ang Nan died in 1691, and the revolt was soon resolved.Song, Jeong Nam, Sự mở rộng lãnh thổ Đại Việt dưới thời Hậu Lê và tính chất, Korean University of Foreign Studies, Seoul, 2010, p.23
After fully subjugating Champa in 1697, the Nguyễn lords sent marquis Nguyễn Hữu Cảnh and a small expedition to annex Prei Nokor, renamed it to Saigon, establishing Vietnamese administrative structures, and explore deep into the lower Mekong Delta from Mỹ Tho to An Giang. King Chey Chettha IV of Cambodia tried to stop the Vietnamese but was defeated by Nguyễn Hữu Cảnh in 1700. In February 1700, he invaded Cambodia from An Giang. In March, the Vietnamese expedition under Cảnh and a Chinese general Trần Thượng Xuyên (Chen Shangchuan) defeated the main Cambodian army at Bích Đôi citadel, king Chey Chettha IV took flight while his nephew Ang Em surrendered to the invaders as the Vietnamese captured Phnom Penh. As a result, Saigon and Long An were officially obtained by the Nguyễn, more Vietnamese settlers moved into the new conquered lands. In 1708, Mạc Cửu of Hà Tiên also pledged loyalty to the Nguyễn lords.
The Muslims rose up and joined the Vietnamese chasing the Cambodians. Due to heavy spring rain, the Muslim segment lost contact with the main army of Nguyễn Cư Trinh, and were surrounded by 10,000 Cambodians at Vô Tà Ân in early 1755. Muslim troops piled carts and wagons into a defensive perimeter and stood their ground against Cambodian attacks until being relieved by Nguyễn Cư Trinh. With the help of mediation by Mạc Thiên Tứ of Hà Tiên, a ceasefire agreement was reached between King Chey Chettha V and Lord Nguyễn Phúc Khoát in 1756: Cambodia ceded Gò Công and Tân An to the Vietnamese, Chey Chettha V was deposed, while Ang Tong was restored as King of Cambodia. Ang Tong offered the Nguyễn two districts of Trà Vinh and Ba Thắc as tributes.Song, Jeong Nam, Sự mở rộng lãnh thổ Đại Việt dưới thời Hậu Lê và tính chất, Korean University of Foreign Studies, Seoul, 2010, p.25
In 1757, Ang Tong died and was succeeded Outey II. With the help of the Nguyễn Lords and the Principality of Hà Tiên, Outey II regained the throne from usurpers. He gave all remaining Mekong Delta lands to Mạc Thiên Tứ, and Mạc Thiên Tứ swapped all these areas to the Nguyễn in exchange for the Mạc clan's total autonomy in Hà Tiên. The new lands were divided into two districts: Rạch Giá and Cà Mau. By 1757, all of today's Mekong Delta including the Cape Cà Mau firmly came under Vietnamese control.
Upon the conclusion of the Cochinchina Campaign in the 1860s, the area became part of Cochinchina, France's first colony in Vietnam, and later, part of French Indochina.
In 1975, North Vietnamese soldiers and Viet Cong soldiers launched a massive invasion in many parts of South Vietnam. While I, II, and III Corps collapsed significantly, IV Corps was still highly intact due to under Major General Nguyễn Khoa Nam overseeing strong military operations to prevent VC taking over any important regional districts. Brigadier General Lê Văn Hưng, the head of 21st Division commander, stayed office in Cần Thơ to continue defending successfully against VC. On 29 April 1975, the last U.S. Consul General Terry McNamara and his diplomats evacuated by marine boat from Cần Thơ to the South China Sea. When the South Vietnamese President Dương Văn Minh ordered unconditional surrender, both ARVN generals in Cần Thơ, General Lê Văn Hưng and Nguyễn Khoa Nam, committed suicide. At Binh Thuy Air Base some ARVN soldiers and air base personnel who defended the air base were evacuated by helicopters and several jet fighters to Thailand shortly after hearing Minh's surrender. Within hours, VC soldiers occupied the base and captured those ARVN and air base personnel who didn't escape. In Mỹ Tho, Brigadier General Trần Văn Hai, who was in charged protecting National Highway 4 (now NH1A) from Saigon to Cần Thơ, committed suicide. Tran was one of the three ARVN generals who refused to be evacuated by American forces when the North Vietnamese soldiers invaded Saigon. Several ARVN soldiers continued to fight against the VC but later either surrendered or disbanded when faced with VC counterattacks.
In the late 1970s, the Khmer Rouge regime attacked Vietnam in an attempt to reconquer the Delta region. This campaign precipitated the Vietnamese invasion of Cambodia and subsequent downfall of the Khmer Rouge.
The Mekong Delta region of Vietnam displays a variety of physical landscapes, but is dominated by flat flood plains in the south, with a few hills in the north and west. This diversity of terrain was largely the product of tectonic uplift and folding brought about by the collision of the Indian Plate and Eurasian Plate tectonic plates about 50 million years ago. The soil of the lower Delta consists mainly of sediment from the Mekong and its tributaries, deposited over thousands of years as the river changed its course due to the flatness of the low-lying terrain.
The present Mekong Delta system has two major distributary channels, both discharging directly into the East Sea. The river carries over 160 million tons of sediment, including 6.5 million tons of sand, each year. Historic sediment loads are estimated to be higher, but have been reduced due to damming for hydropower in the upper reaches of the Mekong River Basin, and sand mining in the riverbed. Sediment is the driving factor in building the delta seaward (progradation), and upward (aggradation) from seasonal flooding, and is counteracted by coastal erosion and sea level rise.
The Holocene history of the Mekong Delta shows delta progradation of about 200 km during the last 6 kyr. During the Middle Holocene the Mekong River was discharging waters into both the East Sea and the Gulf of Thailand. The water entering the Gulf of Thailand was flowing via a palaeochannel located within the western part of the delta; north of the Camau Peninsula. Upper Pleistocene prodeltaic and delta front sediments interpreted as the deposits of the palaeo-Mekong River were reported from central basin of the Gulf of Thailand.
The Mekong Delta is the region with the smallest forest area in Vietnam. or 7.7% of the total area are forested as of 2011. The only provinces with large forests are Cà Mau and An Giang, together accounting for two-thirds of the region's forest area, while forests cover less than 5% of the area of all of the other eight provinces and cities.
From 1973 to 2005, the Mekong Delta's seaward shoreline growth decreased gradually from a mean of 7.8 m/yr to 2.8 m/yr, becoming negative after 2005, with a retreat rate of −1.4 m/yr. The net deltaic land area gain has also been slowing, with the mean rate decreasing from 4.3 km2/yr (1973–1979) to 1.0 km2 yr (1995–2005), and then to −0.05 km2/yr (2005–2015). Thus, in about 2005, the subaerial Mekong Delta transitioned from a constructive mode to an erosional (or destructive) mode.
The duration of inundations at an important road in the city of Cần Thơ is expected to continue to rise from the current total of 72 inundated days per year to 270 days by 2030 and 365 days by 2050. This is attributed to the combined influence of sea-level rise and land subsidence, which occurs at about annually. Several projects and initiatives on local, regional and state levels work to counter this trend and save the Mekong Delta. For example, there exists a programme for integrated coastal management that is supported by Germany and Australia. Additionally, international and local initiatives, including significant environmental funding and legislation like Resolution 120 in 2017, emphasize sustainable management and conservation of , focusing on nature-based solutions such as retrofitting dikes, mangrove restoration, and multi-value farming to mitigate environmental degradation.
In August 2019, a Nature Communications study using an improved measure of elevation estimation, found that the delta was much lower than previous estimates, only a mean above sea level, with 75% of the delta—an area where 12 million people currently live—falling below . It is expected that a majority of the delta will be below sea level by 2050.
The languages spoken in the Mekong Delta are mainly Vietnamese and Khmer language which cover almost the majority of the population. Then there are also various Chinese languages spoken by the Hoa community, as well as the Cham language and Mekong Delta Malay languages which are the lingua franca for the Muslim community there.
The population of the Mekong Delta has been growing relatively slowly in recent years, mainly due to out-migration. The region's population only increased by 471,600 people between 2005 and 2011, while 166,400 people migrated out in 2011 alone. Together with the central coast regions, it has one of the slowest growing populations in the country. Population growth rates have been between 0.3% and 0.5% between 2008 and 2011, while they have been over 2% in the neighbouring southeastern region. Net migration has been negative in all of these years. The region also has a relatively low fertility rate, at 1.8 children per woman in 2010 and 2011, down from 2.0 in 2005.
Rice output in 2011 was 23,186,000t, 54.8% of Vietnam's total output. The strongest producers are Kiên Giang province, An Giang province, and Đồng Tháp province, producing over 3 million tonnes each and almost 11 million tonnes together. Any two of these provinces produce more than the entire Red River Delta. Only three provinces produce less than 1 million tonnes of rice (Bạc Liêu province, Cà Mau province, Bến Tre province).
Despite the region's large offshore fishing fleet, 2/3 (2.13 million tonnes out of Vietnam's total of 2.93) of fishery output actually comes from aquaculture.
December 2015, aquaculture production was estimated at 357 thousand tons, up 11% compared to the same period last year, bringing the total aquaculture production 3516 thousand tons in 2015, up 3.0% compared to the same period. Although aquaculture production has increased overall, aquaculture still faces many difficulties coming from export markets.
The region is served by 4 airports:
However, Ho Chi Minh City's Tan Son Nhat International Airport is another alternative airport which provides more domestic and international destinations. The airport is approximately located 160 km north of Cần Thơ.
The region is home to cải lương, a form of Kinh/Vietnamese folk opera. Cai Luong Singing appeared in Mekong Delta in the early 20th century. Cai Luong Singing is often performed to the accompaniment of guitar and zither. Cai Luong is a kind of play telling a story. This often includes two main parts: the dialogue part and the singing part to express their thoughts and emotions.
The 2004 film The Buffalo Boy is set in Cà Mau province.
Some Vietnamese films on the topic of life in the Mekong Delta attract the attention of a large audience: Tình Mẫu Tử (Mother and child love, 2019), Phận làm dâu (Bride's fate, 2018), etc.
Conquest of the Mekong Delta
Nguyễn dynasty, French and modern period
Geography
Coastal erosion
43-yr average 8.87 −12.79 21.53 −1.66 4.36 43-yr average 2.12 −1.71 1.99 −0.18 2.23
Climate change concerns
Demographics
Provinces
An Giang Rạch Giá Cà Mau Tân Thành Đồng Tháp Mỹ Tho Vĩnh Long Long Châu Cần Thơ Ninh Kiều
Economy
Agriculture
Fishery
Industry and FDI
Infrastructure
Culture
Cuisine
Literature and movies
See also
Further reading
External links
Climate change
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