Mekong

Mekong River
Megaung Myit, แม่น้ำโขง (Maenam Khong), Mékôngk, Tonle Thom, Cửu Long, Mê Kông, 湄公 (Méigōng), ទន្លេរមេគង្គ
River
A view of the Mekong River at Luang Prabang in Laos
Countries	China, Burma (Myanmar), Laos, Thailand, Cambodia, Vietnam
States	Qinghai, Tibet, Yunnan, Shan, Luang Namtha, Bokeo, Oudomxay, Luang Phrabang, Sayabouly, Vientiane, Vientiane, Bolikhamsai, Khammouane, Savannakhet, Salavan, Champasak
Source	Lasagongma Spring
- location	Mt. Guozongmucha, Zadoi, Yushu Tibetan Autonomous Prefecture, Qinghai, China
- elevation	5,224 m (17,139 ft)
- coordinates	33°42.5′N 94°41.7′E
Mouth	Mekong Delta
- elevation	0 m (0 ft)
Length	4,350 km (2,703 mi)
Basin	795,000 km2 (307,000 sq mi)
Discharge	for South China Sea
- average	16,000 m3/s (570,000 cu ft/s)
- max	39,000 m3/s (1,400,000 cu ft/s)

The Mekong is a trans-boundary river in Southeast Asia. It is the world's 12th-longest river and the 7th-longest in Asia. Its estimated length is 4,350 km (2,703 mi), and it drains an area of 795,000 km² (307,000 sq mi), discharging 475 km³ (114 cu mi) of water annually.

From the Tibetan Plateau this river runs through China's Yunnan province, Burma (Myanmar), Laos, Thailand, Cambodia and Vietnam. In 1995, Laos, Thailand, Cambodia and Vietnam established the Mekong River Commission to assist in the management and coordinated use of the Mekong's resources. In 1996 China and Burma (Myanmar) became "dialogue partners" of the MRC and the six countries now work together within a cooperative framework.

The extreme seasonal variations in flow and the presence of rapids and waterfalls in this river have made navigation difficult. The river is a major trading route linking China’s southwestern province of Yunnan to Laos, Burma (Myanmar) and Thailand to the south, an important trade route between western China and Southeast Asia.

Names

In English the river is called "the Mekong River", derived from "Mae Nam Khong" or "Tonle Mekong", a term of both Thai, Lao and Khmer (Cambodia) origin. In Khmer language "Mae" meaning "Big, Mother, Boss or Large" and "Kong" is a short word of "Kongkea" and it means "Water". In the Lao-Khmer-Thai toponymy, all great rivers are considered "mother rivers" signalled by the prefix "mae", meaning "mother", and "nam" for water. In the Mekong's case, Mae Nam Khong means Khong, The Mother of Water. "Khong" or "Kongkea" is derived from the Sanskrit "Ganga", meaning "Sacred Water" or the Ganges. Many Northern Thai and Laos locals refer to it as the "River Khong". Such is the case with the Mae Nam Ping in Chiang Mai which is known as the " Ping River". The Beung Tonle Sap in Cambodia is a similar example – where Beung translates as "Lake", Tonle translates as "Great flowing lake or river" and Sap translates as "Freshwater, tasteless, flavourless and unsalted", making the Tonle Sap River or "Beung Tonle Sap River" an unnecessary repetition of what is in fact the "Sap River Lake".

Since the river flows through a number of countries, it has many different names in local languages:

• Burmese: မဲခေါင်မြစ်, IPA:  [mɛ́ɡàʊɴ mjɪ̰ʔ]
• Chinese: Riverhead: 加果空桑贡玛曲, 扎那曲 and 扎曲 Zā Qū, upper reaches: 澜沧江, 瀾滄江 Láncāng Jiāng ("Turbulent River", "Láncāng" is the same as ' Lan Xang' in Chinese), middle and lower reaches: 湄公河 Méigōng hé.
• Khmer: មេគង្គ Mékôngk [meekoŋ], ទន្លេមេគង្គ Tônlé Mékôngk [tʊənlee meekoŋ], ទន្លេធំ Tônlé Thum [tʊənlee tʰom] ("Great River").
• Lao: ແມ່ນ້ຳຂອງ, [mɛː nâːm kʰɔ̌ːŋ], ນ້ຳຂອງ [nâːm kʰɔ̌ːŋ].
• Thai: แม่น้ำโขง, [mɛ̂ː náːm kʰǒːŋ].
• Tibetan: རྫ་ཆུ་,  Wylie: rDza chu, ZYPY: Za qu
• Vietnamese: Sông Mê Kông (pronounced  [soŋm mekoŋm]), Sông Lớn ("Great River", [soŋm lə̌ːn]), Sông Cửu Long ("Nine Dragons River", [soŋm kɨ̃w lɔŋ]).

Course

The Mekong rises in the "Three Rivers Area" on the Tibetan Plateau in the Sanjiangyuan National Nature Reserve as the Lancang, together with the Yangtze and Yellow (Huang He) Rivers. It flows southwest through Yunnan Province, and through the Three Parallel Rivers Area in the Hengduan Mountains, along with the Salween River (Nujiang in Chinese) and the Yangtze.

After leaving China, it flows southwest and forms the border of Burma (Myanmar) and Laos for about 100 kilometres (62 mi) then turns southeast to briefly form the border of Laos with Thailand. The Mekong then flows east and south into Laos for some 400 kilometres (250 mi) and defines the Laos-Thailand border again for some 850 kilometres (530 mi) as it flows first east, passing in front of the capital of Laos, Vientiane, then turns south through central Southeast Asia. The river leaves the border and flows into Laos shortly before passing the city of Pakse. Thereafter, it runs more or less directly south, crossing into Cambodia.

At Phnom Penh the river is joined on the right bank by the river and lake system the Tonle Sap. When the Mekong is low, the Tonle Sap is a tributary; water flows from the lake and river into the Mekong. When the Mekong floods, the flow reverses; the floodwaters of the Mekong flow up the Tonle Sap.

Immediately after the Sap River joins the Mekong by Phnom Penh, the Bassac River branches off the right (south) bank. The Bassac River is the first and main distributary of the Mekong; thus, this is the beginning of the Mekong Delta. The two rivers, the Bassac to the south and the Mekong to the north, enter Vietnam very soon after this. In Vietnam, the Bassac is called the Hậu River (Sông Hậu or Hậu Giang); the main, northern, branch of the Mekong is called the Sông Tiền or Tiền Giang. In Vietnam, distributaries of the northern branch include the sông (river) Mỹ Tho, the sông Ba Lai, the sông Hàm Luông, and the sông Cổ Chiên.

Drainage basin

The Mekong Basin can be divided into two parts: the 'Upper Mekong Basin' in Tibet and China, and the 'Lower Mekong Basin' from Yunnan downstream from China to the South China Sea. From the point where it rises to its mouth, the most precipitous drop in the Mekong occurs in Upper Mekong Basin, a stretch of some 2,200 km (1,400 mi). Here, it drops 4,500 metres (14,800 ft) before it enters the Lower Basin where the borders of Thailand, Laos, China and Burma (Myanmar) come together in the Golden Triangle. Downstream from the Golden Triangle, the river flows for a further 2,600 km (1,600 mi) through Laos, Thailand and Cambodia before entering the South China Sea via a complex delta system in Vietnam.

Upper Mekong Basin

The Upper Basin makes up 24% of the total area and contributes 15 to 20% of the water that flows into the Mekong River. The catchment here is steep and narrow. Soil erosion has been a major problem and approximately 50% of the sediment in the river comes from the Upper Basin.

In Yunnan province in China, the river and its tributaries are confined by narrow, deep gorges. The tributary river systems in this part of the basin are small. Only 14 have catchment areas that exceed 1,000 km² (390 sq mi), yet the greatest amount of loss of forest cover in the entire river system per square kilometer has occurred in this region due to heavy unchecked demand for natural resources. In the south of Yunnan, in Simao and Xishuangbanna Prefectures, the river changes as the valley opens out, the floodplain becomes wider, and the river becomes wider and slower.

Lower Mekong Basin

Major tributary systems develop in the Lower Basin. These systems can be separated into two groups: tributaries that contribute to the major wet season flows, and tributaries that drain low relief regions of lower rainfall. The first group are left bank tributaries that drain the high-rainfall areas of Lao PDR. The second group are those on the right bank, mainly the Mun and Chi rivers, that drain a large part of Northeast Thailand.

Laos lies almost entirely within the Lower Mekong Basin. Its climate, landscape and land use are the major factors shaping the hydrology of the river. The mountainous landscape means that only 16% of the country is farmed under lowland terrace or upland shifting cultivation. With upland shifting agriculture (slash and burn), soils recover within 10 to 20 years but the vegetation does not. Shifting cultivation is common in the uplands of Northern Laos and is reported to account for as much as 27% of the total land under rice cultivation. As elsewhere in the basin, forest cover has been steadily reduced during the last three decades by shifting agriculture and permanent agriculture. The cumulative impacts of these activities on the river regime have not been measured. However, the hydrological impacts of land-cover changes induced by the Vietnam War were quantified in two sub-catchments of the Lower Mekong River Basin.

Loss of forest cover in the Thai areas of the Lower Basin has been the highest in all the Lower Mekong countries over the past 60 years. On the Korat Plateau, which includes the Mun and Chi tributary systems, forest cover was reduced from 42% in 1961 to 13% in 1993. Although this part of Northeast Thailand has an annual rainfall of more than 1,000 mm, a high evaporation rate means it is classified as a semi arid region. Consequently, although the Mun and Chi Basins drain 15% of the entire Mekong Basin, they only contribute 6% of the average annual flow. Sandy and saline soils are the most common soil types, which makes much of the land unsuitable for wet rice cultivation. In spite of poor fertility, however, agriculture is intensive. Glutinous rice, maize and cassava are the principal crops. Drought is by far the major hydrological hazard in this region.

As the Mekong enters Cambodia, over 95% of the flows have already joined the river. From here on downstream the terrain is flat and water levels rather than flow volumes determine the movement of water across the landscape. The seasonal cycle of changing water levels at Phnom Penh results in the unique “flow reversal” of water into and out of the Great Lake via the Tonle Sap River. Phnom Penh also marks the beginning of the delta system of the Mekong River. Here the mainstream begins to break up into an increasing number of branches.

In Cambodia, the wet rice is the main crop and is grown on the flood plains of the Tonle Sap, Mekong and Bassac (the Mekong delta distributary known as the Hậu in Vietnam) rivers. More than half of Cambodia remains covered with mixed evergreen and deciduous broadleaf forest, but forest cover has decreased from 73% in 1973 to 63% in 1993. Here, the river landscape is flat. Small changes in water level determine the direction of water movement, including the large-scale reversal of flow into and out of the Tonle Sap basin from the Mekong River.

The Mekong Delta in Viet Nam is farmed intensively and has little natural vegetation left. Forest cover is less than 10%. In the Central Highlands of Vietnam, forest cover was reduced from over 95% in the 1950s to around 50% in the mid 1990s. Agricultural expansion and population pressure are the major reasons for land use and landscape change. Both drought and flood are common hazards in the Delta, which many people believe is the most sensitive to upstream hydrological change.

Water flow along its course

Table 1: Basic data on country share of Mekong Basin territory and water flows

	China	Burma (Myanmar)	Lao PDR	Thailand	Cambodia	Vietnam	Total
Area in Basin (km,2)	165,000	24,000	202,000	184,000	155,000	65,000	795,000
Catchment as % of MRB	21	3	25	23	20	8	100
Flow as % of MRB	16	2	35	18	18	11	100

By taking into account hydrological regimes, physiography land use, and existing, planned and potential resource developments, the Mekong is divided into six distinct reaches:

Reach 1: Lancang Jiang or Upper Mekong River in China. In this part of the river, the major source of water flowing into the river comes from melting snow on the Tibetan Plateau. This volume of water is sometimes called the “Yunnan Component” and plays an important role in the low-flow hydrology of the lower mainstream. Even as far downstream as Kratie, the Yunnan Component makes up almost 30% of the average dry season flow. A major concern is that the on-going and planned expansion of dams and reservoirs on the Mekong mainstream in Yunnan could have a significant effect on the low-flow regime of the Lower Mekong Basin system.

Reach 2: Chiang Saen to Vientiane and Nongkhai. This reach is almost entirely mountainous and covered with natural forest, although there has been widespread slash and burn agriculture. Although this reach could hardly be described as “unspoiled”, the hydrological response is perhaps the most natural and undisturbed in all the Lower Basin. Many hydrological aspects of the Lower Basin start to change rapidly at the downstream boundary of this reach.

Reach 3: Vientiane and Nongkhai to Pakse. The boundary between Reach 2 and 3 is where the Mekong hydrology starts to change. Reach 2 is dominated in both wet and dry seasons by the Yunnan Component. Reach 3 is increasingly influenced by contributions from the large left bank tributaries in Laos, namely the Nam Ngum, Nam Theun, Nam Hinboun, Se Bang Fai, Se Bang Hieng and Se Done rivers. The Mun- Chi river system from the right bank in Thailand enters the mainstream within this reach.

Reach 4: Pakse to Kratie. The main hydrological contributions to the mainstream in this reach come from the Se Kong, Se San and Sre Pok catchments. Together, these rivers make up the largest hydrological subcomponent of the Lower Basin. Over 25% of the mean annual flow volume to the mainstream at Kratie comes from these three river basins. They are the key element in the hydrology of this part of the system, especially to the Tonle Sap flow reversal.

Reach 5: Kratie to Phnom Penh. This reach includes the hydraulic complexities of the Cambodian floodplain, the Tonle Sap and the Great Lake. By this stage, over 95% of the total flow has entered the Mekong system. The focus turns from hydrology and water discharge to the assessment of water level, over- bank storage and flooding and the hydrodynamics that determine the timing, duration and volume of the seasonal flow reversal into and out of the Great Lake.

Reach 6: Phnom Penh to the South China Sea. Here the mainstream divides into a complex and increasingly controlled and artificial system of branches and canals. Key features of flow behaviour are tidal influences and salt water intrusion. Every year, 35 to 50% of this reach is flooded during the rainy season. The impact of road embankments and similar infrastructure developments on the movement of this flood water is an increasingly important consequence of development.

Table 2 summarises the mean annual flows along the mainstream. The mean annual flow entering the lower Mekong from China is equivalent to a relatively modest 450 mm depth of runoff. Downstream of Vientiane this increases to over 600 mm as the principal left bank tributaries enter the mainstream, mainly the Nam Ngum and Nam Theun. The flow level falls again, even with the right bank entry of the Mun-Chi system from Thailand. Although the Mun - Chi basin drains 20% of the lower system, average annual runoff is only 250 mm. Runoff in the mainstream increases again with the entry from the left bank of the Se Kong from southern Laos and Se San and Sre Pok from Vietnam and Cambodia.

Table 2: Lower Mekong Mainstream annual flow (1960 to 2004) at selected sites.

Mainstream site	Catchment area (km2)	Mean annual flow as			as % total Mekong
		Discharge m³/s	Volume km3	Runoff (mm)
Chiang Saen	189,000	2,700	85	450	19
Luang Prabang	268,000	3,900	123	460	27
Chiang Khan	292,000	4,200	133	460	29
Vientiane	299,000	4,400	139	460	30
Nongkhai	302,000	4,500	142	470	31
Nakhon Phanom	373,000	7,100	224	600	49
Mukdahan	391,000	7,600	240	610	52
Pakse	545,000	9,700	306	560	67
Stung Treng	635,000	13,100	413	650	90
Kratie	646,000	13,200	416	640	91
Basin Total	760,000	14,500	457	600	100

Flows at Chiang Saen entering the Lower Basin from Yunnan make up about 15% of the wet season flow at Kratie. This rises to 40% during the dry season, even this far downstream. During the wet season, the proportion of average flow coming from Yunnan rapidly decreases downstream of Chiang Saen, from 70% to less than 20% at Kratie. The dry season contribution from Yunnan is much more significant. The major portion of the balance comes from Laos, which points to a major distinction in the low-flow hydrology of the river. One fraction comes from melting snow in China and Tibet and the rest from over-season catchment storage in the Lower Basin. This has implications for the occurrence of drought conditions. For example, if runoff from melting snow in any given year is very low, then flows upstream of Vientiane- Nongkhai would be lower.

In a large river system like the Mekong, seasonal flows can be quite variable from year to year. Although the pattern of the annual hydrograph is fairly predictable, its magnitude is not. The average monthly flows along the mainstream are listed in Table 3, providing an indication of their range and variability from year to year. At Pakse, for example, flood season flows during August would exceed 20,000 cubic metres per second 9 years out of 10, but exceed 34,000 m³/s only 1 year in ten.

Table 3: Mekong Mainstream monthly discharge 1960 to 2004 (m³/s).

Month	Chian Saen	Luang Prabang	Vientiane	Nakhon Phanom	Mukdahan	Pakse	Kratie
Jan	1,150	1,690	1,760	2,380	2,370	2,800	3,620
Feb	930	1,280	1,370	1,860	1,880	2,170	2,730
Mar	830	1,060	1,170	1,560	1,600	1,840	2,290
Apr	910	1,110	1,190	1,530	1,560	1,800	2,220
May	1,300	1,570	1,720	2,410	2,430	2,920	3,640
Jun	2,460	3,110	3,410	6,610	7,090	8,810	11,200
Jul	4,720	6,400	6,920	12,800	13,600	16,600	22,200
Aug	6,480	9,920	11,000	19,100	20,600	26,200	35,500
Sep	5,510	8,990	10,800	18,500	19,800	26,300	36,700
Oct	3,840	5,750	6,800	10,200	10,900	15,400	22,000
Nov	2,510	3,790	4,230	5,410	5,710	7,780	10,900
Dec	1,590	2,400	2,560	3,340	3,410	4,190	5,710

There is little evidence from the last 45 years of data of any systematic changes in the hydrological regime of the Mekong.

Mekong River modifications

The Mekong is already heavily dammed, with many more dams planned and under construction.

Natural history

The Mekong basin is one of the richest areas of biodiversity in the world. Only the Amazon boasts a higher level of biodiversity. Biota estimates for the Greater Mekong Subregion (GMS) include 20,000 plant species, 430 mammals, 1,200 birds, 800 reptiles and amphibians and an estimated 850 fish species. In 2009, 145 new species were described from the Mekong Region, comprising 29 fish species previously unknown to science, two new bird species, ten reptiles, five mammals, 96 plants and six new amphibians. The Mekong Region contains 16 WWF Global 200 ecoregions, the greatest concentration of ecoregions in mainland Asia.

No other river is home to so many species of very large fish. The biggest include the giant river carp (Probarbus jullieni), which can grow up to 1.5 metres (4 ft 11 in) and weigh 70 kilograms (150 lb), the Mekong Freshwater Stingray ( Himantura chaophraya), which can have a wingspan of up to 4.3 metres (14 ft), the giant pangasius (Pangasius sanitwongsei), Siamese giant carp (Catlocarpio siamensis) and the endemic Mekong giant catfish (Pangasianodon gigas), all three of which can grow up to about 3 metres (9 ft 10 in) in length and weigh 300 kilograms (660 lb). All of these are in serious decline, because of dams, flood control and overfishing.

One species of freshwater dolphin, the Irrawaddy Dolphin (Orcaella brevirostris), was once common in the whole of the Lower Mekong but is now very rare.

Among other wetland mammals that have been living in and around the river are the smooth-coated otter (Lutra perspicillata) and fishing cat (Felis viverrina).

The endangered Siamese crocodile (Crocodylus siamensis) occurs in small isolated pockets within the northern Cambodian and Laotian portions of the Mekong River. The Saltwater crocodile (Crocodylus porosus) once ranged from the Mekong Delta up the river into Tonle Sap and beyond but is now extinct in the river, along with being extinct in all of Vietnam and possibly even Cambodia.

The fisheries

Aquatic biodiversity in the Mekong river system is the second highest in the world after the Amazon. The Mekong boasts the most concentrated biodiversity per hectare of any river.

The commercially valuable fish species in the Mekong are generally divided between ‘black fish’, which inhabit low oxygen, slow moving, shallow waters, and ‘white fish’, which inhabit well oxygenated, fast moving, deeper waters. People living within the Mekong river system generate many other sources of food and income from what are often termed ‘other aquatic animals’ (OAAs) such as freshwater crabs, shrimp, snakes, turtles, and frogs.

OAAs account for about 20 percent of the total Mekong catch. When fisheries are discussed, catches are typically divided between the wild capture fishery (i.e. fish and other aquatic animals caught in their natural habitat), and aquaculture (fish reared under controlled conditions). Wild capture fisheries play the most important role in supporting livelihoods. Wild capture fisheries are largely open access fisheries, which poor rural people can access for food and income.

Broadly, there are three types of fish habitats in the Mekong: i) the river, comprising all the main tributaries, rivers in the major flood zone and the Tonle Sap, which altogether yield about 30 percent of wild catch landings; ii) rainfed wetlands outside the river-floodplain zone, comprising mainly rice paddy in formerly forested areas and usually inundated to about 50 cm and yielding about 66 percent of wild catch landings; and iii) large water bodies outside the flood zone, including canals and reservoirs yielding about 4 percent of wild catch landings.

The Mekong Basin has one of the world’s largest and most productive inland fisheries. An estimated 2 million tonnes of fish are landed a year, in addition to almost 500,000 tonnes of other aquatic animals. Aquaculture yields about 2 million tonnes of fish a year.

Hence, the Lower Mekong Basin yields about 4.5 million tonnes of fish and aquatic products annually. The total economic value of the fishery is between USD 3.9 to USD 7 billion a year. Wild capture fisheries alone have been valued at USD 2 billion a year. This value increases considerably when the multiplier effect is included, but estimates vary widely.

An estimated 2.56 million tonnes of inland fish and other aquatic animals are consumed in the lower Mekong every year. Aquatic resources make up between 47 percent and 80 percent of animal protein in rural diets for people who live in the Lower Mekong Basin. Fish are the cheapest source of animal protein in the region and any decline in the fishery is likely to significantly impact nutrition, especially among the poor. The size of this impact has not been established

It is estimated that 40 million rural people, more than two-thirds of the rural population in the Lower Mekong Basin, are engaged in the wild capture fishery. Fisheries contribute significantly to a diversified livelihood strategy for many people, particularly the poor, who are highly dependent on the river and its resources for their livelihoods.

They provide a principal form of income for a large number of people and act as a safety net and coping strategy in times of poor agricultural harvests or other difficulties. In Lao PDR alone, 71 percent of rural households (2.9 million people) rely on fisheries for either subsistence or additional cash income. Around the Tonle Sap Lake in Cambodia, more than 1.2 million people live in fishing communes and depend almost entirely on fishing for their livelihoods.

Navigation

For thousands of years the Mekong River has been an important conduit for people and goods between the many towns situated along its banks. Traditional forms of trade in small boats linking communities continue today, however the river is also becoming an important link in international trade routes, connecting the six Mekong countries to each other, and also to the rest of the world. The Mekong is still a wild river and navigation conditions vary greatly along its length. Broadly, navigation of the river is divided between upper and lower Mekong, with the 'upper' part of the river defined as the stretch north of the Khone Falls in southern Laos; and the 'lower' part as the stretch below these falls.

Narrower and more turbulent sections of water in the upstream parts of the Mekong River, coupled with large annual water level variations continue to present a challenge to navigation. The seasonal variations in water level directly affect trade in this section of the river. Volumes of trade being shipped decrease by more than 50 per cent, primarily due to the reduced draughts available during the low water season (June–January). Despite these difficulties, the Mekong River is already an important link in the transit chain between Kunming and Bangkok with about 300,000 tonnes of goods shipped via this route each year. The volume of this trade is expected to increase by 8–11 per cent per year. Port infrastructure is being expanded to accommodate the expected growth in traffic, with new facilities planned for Chiang Saen port.

In Laos, 50 and 100 DWT vessels are primarily operated for regional trade, the main types of cargo carried are timber, agricultural products and construction materials. Thailand imports a wide variety of products from China, including vegetables, fruit, agricultural products and fertilisers. The main exports from Thailand are dried longan, fish oil, rubber products and consumables. Nearly all the ships carrying cargo to and from Chiang Saen Port are 300 DWT Chinese flag vessels.

Waterborne trade in the lower Mekong countries of Vietnam and Cambodia has grown significantly, with trends in container traffic at Phnom Penh port and general cargo through Can Tho port both showing steady increases until 2009 when a decrease in cargo volumes can be attributed to the global financial crisis and a subsequent decline in demand for the export of garments to the US. In 2009, Mekong trade received a significant boost with the opening of a new deep-water port at Cai Mep in Vietnam. This new port has generated a renewed focus on the Mekong River as a trade route. The Cai Mep container terminals can accom- modate vessels with a draught of 15.2 m, equivalent to the largest container ships in the world. These mother vessels sail directly to Europe or the United States, which means that goods can be shipped internationally to and from Phnom Penh with only a single trans-shipment at Cai Mep.

As an international river, a number of agreements exist between the countries that share the Mekong to enable trade and passage between them. The most important of these, which address the full length of the river, are:

• Agreement between China and Lao PDR on Freight and Passenger Trans- port along the Lancang–Mekong River, adopted in November 1994.
• Agreement on the Cooperation for the Sustainable Development of the Mekong River Basin, Article 9, Freedom of Navigation, 5 April 1995, Chiang Rai.
• Hanoi Agreement between Cambodia and Viet Nam on Waterway Transportation, 13 December 1998.
• Agreement between and among the Governments of the Laos, Thailand, and Vietnam for Facilitation of Cross border Transport of Goods and People, (amended at Yangon, Burma (Myanmar)), signed in Vientiane, 26 November 1999.
• Agreement on Commercial Navigation on Lancang–Mekong River among the governments of China, Laos, Burma (Myanmar) and Thailand, adopted at Tachileik, 20 April 2000.
• Phnom Penh Agreement between Cambodia and Vietnam on the Transit of Goods, 7 September 2000.
• New Agreement on Waterway Transportation between Vietnam and Cambodia, signed in Phnom Penh, 17 December 2009.

Geology

The internal drainage patterns of the Mekong are unusual when compared to those of other large rivers. Most large river systems that drain the interiors of continents, such as the Amazon, Congo, and Mississippi, have relatively simple dendritic tributary networks that resemble a branching tree.

Typically, such patterns develop in basins with gentle slopes where the underlying geological structure is fairly homogenous and stable, exerting little or no control on river morphology. In marked contrast, the tributary networks of the Salween, Yangtze, and particularly the Mekong, are complex with different sub-basins often exhibiting different, and distinct, drainage patterns. These complex drainage systems have developed in a setting where the underlying geological structure is heterogeneous and active, and is the major factor controlling the course of rivers and the landscapes they carve out.

The elevation of the Tibetan Plateau during the Tertiary period was an important factor in the genesis of the south-west monsoon, which is the dominant climatic control influencing the hydrology of the Mekong Basin. Understanding the nature and timing of the elevation of Tibet (and the Central Highlands of Viet Nam) therefore helps explain the provenance of sediment reaching the delta and the Tonle Sap Great Lake today. Studies of the provenance of sediments in the Mekong Delta reveal a major switch in the source of sediments about eight million years ago (Ma). From 36 to 8 Ma the bulk (76%) of the sediments deposited in the delta came from erosion of the bedrock in the Three Rivers Area. From 8 Ma to the present, however, the contribution from the Three Rivers Area fell to 40%, while that from the Central Highlands rose from 11 to 51%. One of the most striking conclusions of provenance studies is the small contribution of sediment from the other parts of the Mekong Basin, notably the Khorat Plateau, the uplands of northern Lao PDR and northern Thailand, and the mountain ranges south of the Three Rivers Area.

The last glacial period came to an abrupt end about 19,000 years ago (ka) when sea levels rose rapidly, reaching a maximum of about 4.5 m above present levels in the early Holocene at about 8 ka. At this time the shoreline of the South China Sea almost reached Phnom Penh and cores recovered from near Angkor Borei contained sediments deposited under the influence of tides, and salt marsh and mangrove swamp deposits. Sediments deposited in the Tonle Sap Great Lake about this time (7.9–7.3 ka) also show indications of marine influence, suggesting a connection to the South China Sea. Although the hydraulic relationships between the Mekong and the Tonle Sap Great Lake systems during the Holocene are not well understood, it is clear that between 9,000 and 7,500 years ago the confluence of the Tonle Sap and the Mekong was in close proximity to the South China Sea.

The present river morphology of the Mekong Delta developed over the last 6,000 years. During this period, the delta advanced 200 km over the continental shelf of the South China Sea, covering an area of more than 62,500 km². From 5.3 to 3.5 ka the delta advanced across a broad embayment formed between higher ground near the Cambodian border and uplands north of Ho Chi Minh City. During this phase of its development the delta was sheltered from the wave action of long-shore currents and was constructed largely through fluvial and tidal processes. At this time the delta was advancing at a rate of 17–18 m per year. After 3.5 ka, however, the delta had built out beyond the embayment and became subject to wave action and marine currents. These deflected deposition south-eastwards in the direction of the Cà Mau Peninsula, which is one of the most recent features of the delta.

For much of its length the Mekong flows through bedrock channels, i.e. channels that are confined or constrained by bedrock or old alluvium in the bed and riverbanks. Geomorphologic features normally associated with the alluvial stretches of mature rivers, such as meanders, oxbow lakes, cut-offs, and extensive floodplains are restricted to a short stretch of the mainstream around Vientiane and downstream of Kratie where the river develops alluvial channels that are free of control exerted by the underlying bedrock.

The Mekong Basin is not normally considered a seismically active area as much of the basin is underlain by the relatively stable continental block. Nonetheless, the parts of the basin in northern Laos, northern Thailand, Burma (Myanmar) and China do experience frequent earthquakes and tremors. The magnitude of these earthquakes rarely exceeds 6.5 on the Richter scale and is unlikely to cause material damage.

History

The difficulty of navigating the river has meant that it has divided, rather than united, the people who live near it. The earliest known settlements date to 2100 BC, with Ban Chiang being an excellent example of that early Iron Age culture. The earliest recorded civilization was the 1st century Indianised-Khmer culture of Funan, in the Mekong Delta. Excavations at Oc Eo, near modern An Giang, have found coins from as far away as the Roman Empire. This was succeeded by the Khmer culture Chenla state by around the 5th century. The Khmer empire of Angkor was the last great Indianized state in the region. From around the time of the fall of the Khmer empire, the Mekong was the frontline between the emergent states of Siam and Tonkin (North Vietnam), with Laos and Cambodia, then situated on the coast, torn between their influence.

The first European to encounter the Mekong was the Portuguese Antonio de Faria in 1540; a European map of 1563 depicts the river, although even by then little was known of the river upstream of the delta. European interest was sporadic: the Spaniards and Portuguese mounted some missionary and trade expeditions, while the Dutch Gerrit van Wuysthoff led an expedition up the river as far as Vientiane in 1641–42.

The French took a serious interest in the region in the mid-19th century, capturing Saigon in 1861, and establishing a protectorate over Cambodia in 1863.

The first systematic exploration began with the French Mekong Expedition led by Ernest Doudard de Lagrée and Francis Garnier, which ascended the river from its mouth to Yunnan between 1866 to 1868. Their chief finding was that the Mekong had too many falls and rapids to ever be useful for navigation. The river's source was located by Pyotr Kuzmich Kozlov in 1900.

From 1893, the French extended their control of the river into Laos, establishing French Indochina by the first decade of the 20th century. This lasted until the First and Second Indochina Wars ended French and American involvement in the region began.

Bridges

Construction of Myanmar-Laos Friendship Bridge is started on February 19, 2013. The bridge will be 691.6 meters long and have 8.5 meters wide two-lane motorway.

The Thai–Lao Friendship Bridge ( Thai: สะพาน มิตรภาพ ไทย-ลาว Saphan Mittaphap Thai-lao) connects Nong Khai city with Vientiane in Laos. The 1,170-metre (3,840 ft)-long bridge opened on April 8, 1994. It has two 3.5-metre (11 ft)-wide lanes with a single railway line in the middle. On March 20, 2004, the Thai and Lao governments agreed to extend the railway to Tha Nalaeng in Laos, this extension has since been completed.

The Second Thai–Lao Friendship Bridge connects Mukdahan to Savannakhet. The two-lane, 12-metre (39 ft)-wide, 1,600-metre (5,200 ft)-long bridge opened to the general public on January 9, 2007.

The Third Thai–Lao Friendship Bridge opened for traffic on November 11, 2011, connecting Nakhon Phanom Province (Thailand) and Thakhek (Laos), as part of Asian Highway 3. The Chinese and Thai governments agreed to build the bridge and share the estimated $33USD million dollar cost of the project.

The Fourth Thai–Lao Friendship Bridge is under construction and will be finished by June 2013. It will link the Chiang Rai Province of Thailand and Ban Houayxay in Laos.

There is one bridge over the Mekong entirely within Laos; unlike the Friendship bridges, this bridge is not a border crossing. It is at Pakse in Champasak Province. It is 1,380 metres (4,528 ft) long, and was completed in 2000. 15°6′19.95″N 105°48′49.51″E).

The Kizuna Bridge is located in Cambodia, in the city of Kompong Cham, on the road linking Phnom Penh with the remote provinces of Ratanakiri and Mondolkiri, and further away Laos. The bridge opened for traffic on December 11, 2001.

The Prek Tamak Bridge, 40 km north of Phnom Penh opened in 2010.

Phnom Penh itself has no bridge under construction yet, although two new bridges have recently opened on the Tonle Sap, and the main bridge on the highway to Ho Chi Minh was duplicated in 2010.

Another new bridge is to be built at Neak Leung on the Phnom Penh to Ho Chi Minh highway with Japanese government assistance, anticipated to be opened in 2014.

In Vietnam, since the year 2000 My Thuan Bridge (Mỹ Thuận), crosses the first channel—the left, main branch of the Mekong, the Sông Tiền or Tiền Giang—a dozen km ahead of Vinh Long (Vĩnh Long) and since 2008 Rach Mieu Bridge (Rạch Miễu) crosses it a dozen km ahead of de My Tho (Mỹ Tho), between the provinces de Tien Giang (Tiền Giang) and Ben Tre (Bến Tre).

Can Tho Bridge (Cần Thơ), crosses the second channel—the right, main distributary of the Mekong, the Bassac (Song Hau). Inaugurated in 2010, it is the longest main span cable-stayed bridge in Southeast Asia.

Protected areas

• The headwaters of the Mekong in Zadoi County, Qinghai, China, are protected in Sanjiangyuan National Nature Reserve. The name Sanjiangyuan means "the Sources of the Three Rivers"; the reserve also includes the headwaters of the Yellow River and the Yangtze.
• The section of the river flowing through deep gorges in Yunnan province is part of the Three Parallel Rivers of Yunnan Protected Areas; a UNESCO World Heritage Site.
• The Tonle Sap Biosphere Reserve in Cambodia contains the largest lake in Southeast Asia. It is a UNESCO Biosphere reserve.

Miscellany

• Balls of light are observable from time to time rising from the water's surface in the stretch of the river near Vientiane or Nong Khai. These are sometimes referred to as Naga fireballs. The locals attribute the phenomenon to Phaya Naga, Mekong Dragons.
• The low tide level of the river in Cambodia is lower than the high tide level out at sea, and the flow of the Mekong inverts with the tides throughout its stretch in Vietnam and up to Phnom Penh. The very flat Mekong Delta area in Vietnam is thus prone to flooding, especially in the provinces of An Giang and Dong Thap (Đồng Tháp), near the Cambodian border.
• A South- and Southeast Asian regional association, the Mekong-Ganga Cooperation, is named after both this river and the Ganges river.