Understand · Environment
How the delta works, and what is changing
A plain-language guide to the four forces that shape the Mekong Delta — the sediment that built it, the salt that pushes in each spring, the slow sinking of the land, and the autumn flood — with every figure dated and sourced.
A delta built by mud
A delta is a pile of sediment. The Mekong carried silt and sand down from the mountains of China, Laos and Cambodia for thousands of years and dropped it where the current slowed near the sea, building a plain that is still extraordinarily low. In 2019 a team of researchers produced a new elevation model and found the delta's mean height to be about 0.8 m above sea level, far lower than the 2.6 m previously assumed.
That number explains a great deal of what you see on a trip. Dykes around fields, sluice gates on canals and houses raised on posts are all ways of living a few tens of centimetres above the water. It also explains why small changes — a little less sediment, a little more sinking, a slightly higher sea — matter so much here.
Sources: Minderhoud et al., Nature Communications, 28 August 2019 · checked .
Less sediment
A delta stays above water only if new sediment keeps arriving to replace what settles and erodes. According to figures from the Mekong River Commission reported in 2019, the river carried about 160 million tonnes of sediment a year on average before the first dam in 1990, and about 80 million tonnes by 2019. The same report projected a further halving if eleven large dams and more than a hundred tributary dams are built by 2040. Some research goes further: a model by a team led at UC Berkeley, cited in Vietnamese reporting in 2025, suggested dams could cut the sediment reaching the Tien and Hau rivers by up to 96%. That is a modelled scenario, not a measurement, and we present it as such.
Sand mining in the rivers, the same 2025 reporting notes, is another cause of bank and coastal erosion. On the coast, the result is visible: a 2022 report counted about 286 km of the delta's 744 km of coastline eroding or severely eroding.
Sources: Việt Nam News citing the Mekong River Commission, 7 November 2019; VnEconomy, 6 March 2025 · checked .
A sinking surface
At the same time the land is sinking. Researchers and Vietnamese reporting name groundwater pumping as a major cause: it compacts the soft layers underneath. Reporting in March 2025, drawing on international studies, a research group at Utrecht University and measurements by the Ministry of Natural Resources and Environment, gave an average subsidence rate of about 0.96 cm a year over roughly the past decade. The 2019 elevation study put the delta-wide average above 1.1 cm a year, with more than 2.5 cm a year in places where pumping is heavy.
A centimetre a year sounds small. Set it against a mean height of 0.8 m and it is the fastest-moving number in this page. A Ministry scenario published in 2020 estimated that a 1 m rise in sea level by the end of the century would leave nearly 40% of the delta's land under water.
Sources: VnEconomy, 6 March 2025; Minderhoud et al., Nature Communications, 28 August 2019 · checked .
Salt in the dry season
Every dry season the river runs low and the sea pushes up the mouths. How far depends on how much water comes down from upstream, on the tides and on how the gates and canals are managed. The national forecasting centre publishes bulletins through the season. Its bulletin of 10 March 2026 forecast the peak for March and April and put salinity of 4 parts per thousand at:
| River or mouth | Distance inland with 4‰ salinity, spring 2026 |
|---|---|
| Vam Co | 40–50 km |
| Cua Tieu and Cua Dai (Tien River mouths) | 25–30 km |
| Ham Luong | 30–35 km |
| Co Chien | 35–40 km |
| Hau | 35–42 km |
The same bulletin rated the season below both 2024–25 and the multi-year average. The worst recent year was 2020: the agriculture ministry's review found 10 of 13 delta provinces affected, the 4 g/l line covering 24.5% of the region — more than 50,300 ha more than in 2016 — and salt arriving nearly three months early and lasting two to two and a half times longer than in the previous extreme year. The provinces most exposed are the coastal ones: in pre-2025 names, Long An, Tien Giang, Ben Tre, Tra Vinh, Soc Trang, Bac Lieu, Ca Mau and Kien Giang.
Sources: National Center for Hydro-Meteorological Forecasting, bulletin of 10 March 2026; Tuổi Trẻ, 20 June 2020, reporting the agriculture ministry's review · checked .
The autumn flood
Upstream the problem is the opposite. Each year from late summer, floodwater from Cambodia spreads over the upper delta around Chau Doc and the Plain of Reeds. For centuries farmers planted around it, and the flood brought fish and fresh sediment to the fields. Today high dykes keep it out of many areas so that farmers can plant a third rice crop. Provinces plan around this: An Giang's 2024 plan for the autumn–winter crop placed no rice where dykes do not fully control floods.
The flood still matters. In early October 2025 the agriculture and environment ministry forecast a peak for 8–13 October of 3.70–3.90 m at Tan Chau and 3.50–3.70 m at Chau Doc, well below the records of 5.06 m and 4.90 m set in 2000, and warned of flooding in the central urban areas of Can Tho and Vinh Long at the highest tides.
Sources: An Giang Department of Agriculture, plan 80/KH-SNNPTNT, 15 July 2024; Ministry of Agriculture and Environment, 3 October 2025 · checked .
What it means for food
The delta covers about 12.8% of Vietnam's land and produces more than half of its rice, about 95% of its rice exports, 65% of its fruit exports and 60% of its seafood exports. Reporting in May 2026 noted that rice area is falling while fruit and aquaculture grow, and that the national programme for one million hectares of high-quality, low-emission rice by 2030 aims at quality and lower emissions rather than more land. On the coast, some rice fields have become brackish ponds. Upstream, high dykes allow more crops but trap sediment outside the fields. Every trip on this site looks at one part of that trade-off.
Sources: VnEconomy, 7 May 2026 · checked .
How we choose figures
- Official or primary sources first: government bulletins, ministry reviews, provincial plans, peer-reviewed research, the national tourism authority
- Every figure carries its date. A salinity figure from 2026 and one from 2020 tell different stories
- Modelled projections are labelled as projections
- When sources disagree we say so, or we leave the number out
- When a newer official figure appears, we replace the old one and change the date
See these forces on the ground on Water and Salt (coast and salinity) or the Delta Study Programme (flood, dykes and fish). The Ben Tre coast and Chau Doc pages describe the places.
Common questions
Questions travellers ask most
Is the Mekong Delta really sinking?
Yes, on average by around a centimetre a year according to studies reported in 2019 and 2025, faster in places where groundwater is pumped heavily. Combined with a mean height of about 0.8 m, that is the main long-term risk.
Is salinity getting worse every year?
Not every year. The 2025–26 season was rated below the multi-year average, while 2016 and 2020 were extreme. It varies with upstream flows and tides, which is why we always give the year.
Are the dams the only cause of sediment loss?
No. Sand mining in the rivers is also named as a cause of erosion. The dams are the largest factor in the figures we cite.
Can visitors see any of this?
Yes: eroded shorelines, closed sluice gates, rain tanks, flood marks on walls, fields turned into ponds. The trips are built to show them.
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Chau Doc: the autumn flood, fish farms, the Cham, Sam Mountain and Tra Su.
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Tell us what you want to understand
A month, the number of travellers and one line about what interests you are enough to start. We reply by email with questions or a draft programme with stops, hotels and road hours.