Xi Jiang
The Xi Jiang at Zhaoqing with Gaoyao opposite
The Pearl River system including the Xi River
Origin	Gui Jiang and Xun Jiang in Wuzhou
Mouth	The Pearl River Delta on the South China Sea
Basin countries	China and Vietnam
Avg. discharge	7,410 cubic metres per second (262,000 cu ft/s)[1]
Left tributaries	He Jiang

The Xi River (Chinese: 西江,; pinyin: Xī Jiāng; literally "West River"; Postal map spelling: Si Kiang) is the western tributary of the Pearl River in China. It is formed by the confluence of the Gui and Xun Rivers in Wuzhou, Guangxi. It then flows east through Guangdong, and enters the Pearl River Delta just east of the Lingyang Gorge in Zhaoqing. The main branch of the Xi River flows southeast through the delta entering the South China Sea at Modao Men, just west of Macau. The major cities along the Xi include Wuzhou, Zhaoqing, and Jiangmen.

The other two main tributaries of Pearl River are the Dongjiang River (literally, the East River) and Beijiang River (the Northern River).

The Xi River is navigable for its entire length. It is a commercial waterway of southern China, and links the delta cities to the interior. Over two thousand years ago, the Lingqu Canal was dug, connecting the Xi River basin (the Li River, which is a tributary of the Gui River with the Xiang River, which flows into the Yangtze, thus providing a continuous waterway from the Pearl River Delta to the Yangtze Valley.

The entire Xi River system is the largest of the Pearl's tributaries, being 2,197 km, and its volume of flow is second in China only to that of the Yangtze River. It supplies water to many places in Guangxi, Guangdong and Macau.

Other transliterations of the River's name include Hsi River and Hsi Chiang.

Another Xi River is a minor tributary of the Jiulong River northwest of Xiamen.

Xi River system[link]

Major cities along the river[link]

• Wuzhou
• Zhaoqing
• Jiangmen

References[link]

A river is a natural watercourse,^[1] usually freshwater, flowing towards an ocean, a lake, a sea, or another river. In a few cases, a river simply flows into the ground or dries up completely before reaching another body of water. Small rivers may also be called by several other names, including stream, creek, brook, rivulet, tributary and rill. There are no official definitions for generic terms, such as river, as applied to geographic features,^[2] although in some countries or communities a stream may be defined by its size. Many names for small rivers are specific to geographic location; one example is "burn" in Scotland and northeast England. Sometimes a river is said to be larger than a creek,^[3] but this is not always the case, because of vagueness in the language.^[4]

Rivers are part of the hydrological cycle. Water within a river is generally collected from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, and the release of stored water in natural ice and snowpacks (e.g., from glaciers). Potamology is the scientific study of rivers.

Topography[link]

Melting toe of Athabasca Glacier, Jasper National Park, Alberta, Canada.

The water in a river is usually confined to a channel, made up of a stream bed between banks. In larger rivers there is also a wider floodplain shaped by flood-waters over-topping the channel. Flood plains may be very wide in relation to the size of the river channel. This distinction between river channel and floodplain can be blurred especially in urban areas where the floodplain of a river channel can become greatly developed by housing and industry.

The term upriver refers to the direction leading to the source of the river, which is against the direction of flow. Likewise, the term downriver describes the direction towards the mouth of the river, in which the current flows

The river channel typically contains a single stream of water, but some rivers flow as several interconnecting streams of water, producing a braided river. Extensive braided rivers are now found in only a few regions worldwide, such as the South Island of New Zealand. They also occur on peneplains and some of the larger river deltas. Anastamosing rivers are similar to braided rivers and are also quite rare. They have multiple sinuous channels carrying large volumes of sediment.

The River Cam from the Green Dragon Bridge, Cambridge UK

Nile River delta, as seen from Earth orbit. The Nile is an example of a wave-dominated delta that has the classic Greek letter delta (Δ) shape after which river deltas were named.

A river flowing in its channel is a source of energy which acts on the river channel to change its shape and form. In 1757, the German hydrologist Albert Brahms empirically observed that the submerged weight of objects that may be carried away by a river is proportional to the sixth power of the river flow speed.^[5] (This formulation is also sometimes called Airy's law.^[6]) Thus, if the speed of flow were doubled, the flow would dislodge objects with 64 times as much submerged weight. In mountainous torrential zones this can be seen as erosion channels through hard rocks and the creation of sands and gravels from the destruction of larger rocks. In U-shaped glaciated valleys, the subsequent river valley can often easily be identified by the V-shaped channel that it has carved. In the middle reaches where the river may flow over flatter land, meanders may form through erosion of the river banks and deposition on the inside of bends. Sometimes the river will cut off a loop, shortening the channel and forming an oxbow lake or billabong. Rivers that carry large amounts of sediment may develop conspicuous deltas at their mouths, if conditions permit. Rivers whose mouths are in saline tidal waters may form estuaries.

Throughout the course of the river, the total volume of water transported downstream will often be a combination of the free water flow together with a substantial contribution flowing through sub-surface rocks and gravels that underlie the river and its floodplain (called the hyporheic zone). For many rivers in large valleys, this unseen component of flow may greatly exceed the visible flow.

Subsurface streams[link]

Most but not all rivers flow on the surface. Subterranean rivers flow underground in caves or caverns. Such rivers are frequently found in regions with limestone geologic formations. Subglacial streams are the braided rivers that flow at the beds of glaciers and ice sheets, permitting meltwater to be discharged at the front of the glacier. Because of the gradient in pressure due to the overlying weight of the glacier, such streams can even flow uphill.

Permanence of flow[link]

An intermittent river (or ephemeral river) only flows occasionally and can be dry for several years at a time. These rivers are found in regions with limited or highly variable rainfall, or can occur because of geologic conditions such as having a highly permeable river bed. Some ephemeral rivers flow during the summer months but not in the winter. Such rivers are typically fed from chalk aquifers which recharge from winter rainfall. In the UK these rivers are called Bournes and give their name to place such as Bournemouth and Eastbourne.

Classification[link]

Rivers have been classified by many criteria including their topography, their biotic status, their relevance to white water rafting or canoeing activities.

Topographical classification[link]

Rivers can generally be classified as either alluvial, bedrock, or some mix of the two. Alluvial rivers have channels and floodplains that are self-formed in unconsolidated or weakly consolidated sediments. They erode their banks and deposit material on bars and their floodplains. Bedrock rivers form when the river downcuts through the modern sediments and into the underlying bedrock. This occurs in regions that have experienced some kind of uplift (thereby steepening river gradients) or in which a particular hard lithology causes a river to have a steepened reach that has not been covered in modern alluvium. Bedrock rivers very often contain alluvium on their beds; this material is important in eroding and sculpting the channel. Rivers that go through patches of bedrock and patches of deep alluvial cover are classified as mixed bedrock-alluvial.

Alluvial rivers can be further classified by their channel pattern as meandering, braided, wandering, anastomose, or straight. The morphology of an alluvial river reach is controlled by a combination of sediment supply, substrate composition, discharge, vegetation, and bed aggradation.

At the turn of the 20th century William Morris Davis devised the "cycle of erosion" method of classifying rivers based on their "age". Although Davis's system is still found in many books today, after the 1950s and 1960s it became increasingly criticized and rejected by geomorphologists. His scheme did not produce testable hypotheses and was therefore deemed non-scientific.^[7] Examples of Davis's river "ages" include:

• Youthful river: A river with a steep gradient that has very few tributaries and flows quickly. Its channels erode deeper rather than wider. Examples include the Brazos, Trinity and Ebro rivers.

• Mature river: A river with a gradient that is less steep than those of youthful rivers and flows more slowly. A mature river is fed by many tributaries and has more discharge than a youthful river. Its channels erode wider rather than deeper. Examples include the Mississippi, Saint Lawrence, Danube, Ohio, Thames and Paraná rivers.

• Old river: A river with a low gradient and low erosive energy. Old rivers are characterized by flood plains. Examples include the Yellow, Ganges, Tigris, Euphrates, Indus and Nile rivers.

• Rejuvenated river: A river with a gradient that is raised by tectonic uplift.

The way in which a river's characteristics vary between the upper course and lower course of a river are summarized by the Bradshaw model. Power-law relationships between channel slope, depth, and width are given as a function of discharge by "river regime".

Biotic classification[link]

There are very many systems of classification based on biotic conditions typically assigning classes from the most oligotrophic or unpolluted through to the most eutrophic or polluted.^[8] Other systems are based on a whole eco-system approach such as developed by the New Zealand Ministry for the Environment.^[9] In Europe, the requirements of the Water Framework Directive has led to the development of a wide range of classification methods including classifications based on fishery status^[10] A system of river zonation used in francophone communities^[11][12] divides rivers into three primary zones:

• The crenon is the uppermost zone at the source of the river. It is further divided into the eucrenon (spring or boil zone) and the hypocrenon (brook or headstream zone). These areas are characterized by low temperatures, reduced oxygen content and slow moving water.
• The rhithron is the upstream portion of the river that follows the crenon. It is characterized by relatively cool temperatures, high oxygen levels, and fast, turbulent flow.
• The potamon is the remaining downstream stretch of river. It is characterized by warmer temperatures, lower oxygen levels, slow flow and sandier bottoms.

Whitewater classification[link]

The International Scale of River Difficulty is used to rate the challenges of navigation—particularly those with rapids. Class I is the easiest and Class VI is the hardest.

Stream order classification[link]

The Strahler Stream Order ranks rivers based on the connectivity and hierarchy of contributing tributaries. Headwaters are first order while the Amazon River is twelfth order. Approximately 80% of the rivers and streams in the world are of the first and second order.

Uses[link]

Leisure activities on the River Avon at Avon Valley Country Park, Keynsham, United Kingdom. A boat giving trips to the public passes a moored private boat.

Rivers have been used as a source of water, for obtaining food, for transport, as a defensive measure, as a source of hydropower to drive machinery, for bathing, and as a means of disposing of waste.

Rivers have been used for navigation for thousands of years. The earliest evidence of navigation is found in the Indus Valley Civilization, which existed in northwestern Pakistan around 3300 BC.^[13] Riverine navigation provides a cheap means of transport, and is still used extensively on most major rivers of the world like the Amazon, the Ganges, the Nile, the Mississippi, and the Indus. Since river boats are often not regulated, they contribute a large amount to global greenhouse gas emissions, and to local cancer due to inhaling of particulates emitted by the transports.^[14][15]

In some heavily forested regions such as Scandinavia and Canada, lumberjacks use the river to float felled trees downstream to lumber camps for further processing, saving much effort and cost by transporting the huge heavy logs by natural means.

Rivers have been a source of food since pre-history.^[16] They can provide a rich source of fish and other edible aquatic life, and are a major source of fresh water, which can be used for drinking and irrigation. It is therefore no surprise to find most of the major cities of the world situated on the banks of rivers. Rivers help to determine the urban form of cities and neighbourhoods and their corridors often present opportunities for urban renewal through the development of foreshoreways such as riverwalks. Rivers also provide an easy means of disposing of waste-water and, in much of the less developed world, other wastes.

Watermill in Belgium

Fast flowing rivers and waterfalls are widely used as sources of energy, via watermills and hydroelectric plants. Evidence of watermills shows them in use for many hundreds of years such as in Orkney at Dounby Click Mill. Prior to the invention of steam power, water-mills for grinding cereals and for processing wool and other textiles were common across Europe. In the 1890s the first machines to generate power from river water were established at places such as Cragside in Northumberland and in recent decades there has been a significant increase in the development of large scale power generation from water, especially in wet mountainous regions such as Norway.

The coarse sediments, gravel, and sand, generated and moved by rivers are extensively used in construction. In parts of the world this can generate extensive new lake habitats as gravel pits re-fill with water. In other circumstances it can destabilise the river bed and the course of the river and cause severe damage to spawning fish populations which rely on stable gravel formations for egg laying.

In upland rivers, rapids with whitewater or even waterfalls occur. Rapids are often used for recreation, such as whitewater kayaking.

Rivers have been important in determining political boundaries and defending countries. For example, the Danube was a long-standing border of the Roman Empire, and today it forms most of the border between Bulgaria and Romania. The Mississippi in North America and the Rhine in Europe are major east-west boundaries in those continents. The Orange and Limpopo Rivers in southern Africa form the boundaries between provinces and countries along their routes.

Ecosystem[link]

The organisms in the riparian zone respond to changes in river channel location and patterns of flow. The ecosystem of rivers is generally described by the River continuum concept, which has some additions and refinements to allow for spatial (dams, waterfalls) and temporal (extensive flooding). The basic idea is that the river can be described as a system that is continuously changing along its length in the physical parameters, the availability of food particles and the composition of the ecosystem. The food (energy) that is the leftover of the upstream part is being utilized downstream.

The general pattern is that the first order streams contain particulate matter (decaying leaves from the surrounding forests), which is processed there by shredders like Plecoptera larvae. The leftovers of the shredders are utilized by collectors, such as Hydropsychidae, and further downstream algae that create the primary production become the main foodsource of the organisms. All changes are gradual and the distribution of each species can be described as a normal curve with the highest density where the conditions are optimal. In rivers succession is virtually absent and the composition of the ecosystem stays fixed in time.

Chemistry[link]

The chemistry of rivers is complex and depends on inputs from the atmosphere, the geology through which it travels and the inputs from man's activities. The chemistry of the water has a large impact on the ecology of that water for both plants and animals and it also affects the uses that may be made of the river water. Understanding and characterising river water chemistry requires a well designed and managed sampling and analysis.

Like many other Aquatic ecosystems, rivers too are under increasing threat of pollution. According to a study of the WWF's Global Freshwater Programme, the 10 most polluted rivers are: Ganges, Indus, Yangtze, Salween-Nu, Mekong-Lancang, Rio Grande/Rio Bravo, Río de la Plata, Danube, Nile-Lake Victoria, and the Murray-Darling.^[17]

Brackish water[link]

Some rivers generate brackish water by having their river mouth in the ocean. This, in effect creates a unique environment in which certain species are found.

Flooding[link]

Flash flooding caused by heavy rain falling in a short amount of time

Flooding is a natural part of a river's cycle. The majority of the erosion of river channels and the erosion and deposition on the associated floodplains occur during flood stage. In many developed areas, human activity has changed river channel form, altering different magnitudes and frequencies of flooding. Some examples of this are the building of levees, the straightening of channels, and the draining of natural wetlands. In many cases human activities in rivers and floodplains have dramatically increased the risk of flooding. Straightening rivers allows water to flow more rapidly downstream increasing the risk of flooding places further downstream. Building on flood plains removes flood storage which again exacerbates downstream flooding. The building of levees may only protect the area behind the levees and not those further downstream. Levees and flood-banks can also increase flooding upstream because of back-water pressure as the upstream water has to squeeze between the levees.

Flow[link]

Studying the flows of rivers is one aspect of hydrology.^[18]

Direction[link]

A common misconception is that most, or even all, rivers flow from north to south.^[19][20][21] Rivers in fact flow downhill regardless of compass direction. Sometimes downhill is from north to south, but equally it can be from south to north, and usually is a complex meandering path involving all directions of the compass.^[22][23][24] Three of the ten longest rivers in the world—the Nile, Yenisei, and Ob—flow north, as do other major rivers such as the Rhine, Mackenzie, and Nelson.

Rivers flowing downhill, from river source to river mouth, do not necessarily take the shortest path. For alluvial streams, straight and braided rivers have very low sinuosity and flow directly down hill, while meandering rivers flow from side to side across a valley. Bedrock rivers typically flow in either a fractal pattern, or a pattern that is determined by weaknesses in the bedrock, such as faults, fractures, or more erodible layers.

Rate[link]

Volumetric flow rate, also called discharge, volume flow rate, and rate of water flow, is the volume of water which passes through a given cross-section of the river channel per unit time. It is typically measured in cubic meters per second (cumec) or cubic feet per second (cfs), where 1 m³/s = 35.51 ft³/s; it is sometimes also measured in litres or gallons per second.

Volumetric flow rate can be thought of as the mean velocity of the flow through a given cross-section, times that cross-sectional area. Mean velocity can be approximated through the use of the Law of the Wall. In general, velocity increases with the depth (or hydraulic radius) and slope of the river channel, while the cross-sectional area scales with the depth and the width: the double-counting of depth shows the importance of this variable in determining the discharge through the channel.

Sediment yield[link]

Sediment yield is the total quantity of particulate matter (suspended or bedload) reaching the outlet of a drainage basin over a fixed time frame. Yield is usually expressed as kilograms per square kilometre per year. Sediment delivery processes are affected by a myriad of factors such as drainage area size, basin slope, climate, sediment type (lithology), vegetation cover, and human land use / management practices. The theoretical concept of the 'sediment delivery ratio' (ratio between yield and total amount of sediment eroded) captures the fact that not all of the sediment eroded within a catchment reaches the outlet (due to, for example, deposition on floodplains). Such storage opportunities are typically increased in catchments of larger size, thus leading to a lower yield and sediment delivery ratio.

Management[link]

River bank repair

Rivers are often managed or controlled to make them more useful, or less disruptive, to human activity.

• Dams or weirs may be built to control the flow, store water, or extract energy.
• Levees, known as dikes in Europe, may be built to prevent river water from flowing on floodplains or floodways.
• Canals connect rivers to one another for water transfer or navigation.
• River courses may be modified to improve navigation, or straightened to increase the flow rate.

River management is a continuous activity as rivers tend to 'undo' the modifications made by people. Dredged channels silt up, sluice mechanisms deteriorate with age, levees and dams may suffer seepage or catastrophic failure. The benefits sought through managing rivers may often be offset by the social and economic costs of mitigating the bad effects of such management. As an example, in parts of the developed world, rivers have been confined within channels to free up flat flood-plain land for development. Floods can inundate such development at high financial cost and often with loss of life.

Rivers are increasingly managed for habitat conservation, as they are critical for many aquatic and riparian plants, resident and migratory fishes, waterfowl, birds of prey, migrating birds, and many mammals.

Gallery[link]

• 

  The Irrawaddy River is in a fairly untamed condition, with wide-reaching "arms and fingers" leading off the main water-flow

• 

  A false-color satellite photograph of the Amazon River in Brazil

See also[link]

Wikimedia Commons has media related to: River

Look up river in Wiktionary, the free dictionary.

	Environment portal
	Ecology portal

References[link]

Further reading[link]

• Jeffrey W. Jacobs. "Rivers, Major World". Water Encyclopaedia. http://www.waterencyclopedia.com/Re-St/Rivers-Major-World.html. 
• Luna B. Leopold (1994). A View of the River. Harvard University Press. ISBN 0-674-93732-5. OCLC 28889034. ISBN.  — a non-technical primer on the geomorphology and hydraulics of water.

External links[link]

• River Network - Connecting people, saving rivers (Environmental organization)

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Ho Chi Minh
Portrait c. 1946
Chairman of the Workers' Party of Vietnam
In office 19 February 1951 – 2 September 1969
Preceded by	Position established
Succeeded by	Post abolished
First Secretary of the Workers' Party of Vietnam
In office 1 November 1956 – 10 September 1960
Preceded by	Trường Chinh
Succeeded by	Lê Duẩn
President of the Democratic Republic of Vietnam
In office 2 September 1945 – 2 September 1969
Preceded by	Position established
Succeeded by	Tôn Đức Thắng
Prime Minister of the Democratic Republic of Vietnam
In office 2 September 1945 – 20 September 1955
Preceded by	Position established
Succeeded by	Phạm Văn Đồng
Personal details
Born	Nguyễn Sinh Cung (1890-05-19)19 May 1890 Nghệ An Province, French Indochina
Died	2 September 1969(1969-09-02) (aged 79) Hanoi, Democratic Republic of Vietnam
Nationality	Vietnamese
Political party	Workers’ Party of Vietnam
Signature

This article contains Vietnamese text. Without proper rendering support, you may see question marks, boxes, or other symbols instead of chữ Nôm, chữ Hán and chữ Quốc Ngữ.

Hồ Chí Minh (Vietnamese pronunciation: [hô cǐ miɲ] (Vietnamese pronunciation: [hô̤ tɕǐmɪŋ] ( listen)); 19 May 1890 – 2 September 1969), born Nguyễn Sinh Cung and also known as Nguyễn Tất Thành and Nguyễn Ái Quốc, was a Vietnamese Stalinist revolutionary leader who was prime minister (1945–1955) and president (1945–1969) of the Democratic Republic of Vietnam (North Vietnam). He was a key figure in the foundation of the Democratic Republic of Vietnam in 1945, as well as the People's Army of Vietnam (PAVN) and the Việt Cộng (NLF or VC) during the Vietnam War.

He led the Việt Minh independence movement from 1941 onward, establishing the communist-governed Democratic Republic of Vietnam in 1945 and defeating the French Union in 1954 at Điện Biên Phủ. He officially stepped down from power in 1955 due to health problems, but remained a highly visible figurehead and inspiration for Vietnamese fighting for his cause – a united, independent Vietnam – until his death. After the war, Saigon, the capital of Republic of Vietnam, was renamed Hồ Chí Minh City in his honor.

Early life[link]

Nguyễn Sinh Cung was born in 1890 in the village of Hoàng Trù, his mother's hometown. From 1895, he grew up in his father's hometown of Kim Liên, Nam Đàn, Nghệ An Province. He had three siblings: his sister Bạch Liên (or Nguyễn Thị Thanh), a clerk in the French Army; his brother Nguyễn Sinh Khiêm (or Nguyễn Tất Đạt), a geomancer and traditional herbalist; and another brother (Nguyễn Sinh Nhuận) who died in his infancy. As a young child, Nguyễn studied with his father before more formal classes with a scholar named Vuong Thuc Do. Nguyễn quickly mastered Chinese writing, a requisite for any serious study of Confucianism, while honing his colloquial Vietnamese writing.^[1] In addition to his studious endeavors, he was fond of adventure, and loved to fly kites and go fishing.^[1] Following Confucian tradition, at the age of 10, his father gave him a new name: Nguyễn Tất Thành (“Nguyễn the Accomplished”).

Nguyễn’s father, Nguyễn Sinh Sắc, was a Confucian scholar and teacher, and later an imperial magistrate in the small remote district of Binh Khe (Qui Nhơn). He was demoted for abuse of power after an influential local figure died several days after receiving 100 strokes of the cane as punishment for an infraction.^[2] In deference to his father, Nguyễn received a French education, attended lycée in Huế, the alma mater of his later disciples, Phạm Văn Đồng and Võ Nguyên Giáp. He later left his studies and chose to teach at Dục Thanh school in Phan Thiết.

In the USA[link]

In 1911, working as the cook's helper on a ship, Nguyễn traveled to the United States. From 1912-13, he lived in New York (Harlem) and Boston, where he worked as a baker at the Parker House Hotel. Among a series of menial jobs, he claimed to have worked for a wealthy family in Brooklyn between 1917–18, and for General Motors as a line manager. It is believed that, while in the United States, he made contact with Korean nationalists, an experience that developed his political outlook.^[3]

In England[link]

At various points between 1913 and 1919, Nguyễn lived in West Ealing, and later in Crouch End, Hornsey. He reportedly worked as a chef at the Drayton Court Hotel in West Ealing.^[4] It is claimed that Nguyễn trained as a pastry chef under Auguste Escoffier at the Carlton Hotel in the Haymarket, Westminster, but there is no evidence to support this.^[3] However, the wall of New Zealand House, home of the New Zealand High Commission, which now stands on the site of the Carlton Hotel, displays a blue plaque, stating that Nguyễn worked there in 1913 as a waiter.

Political education in France[link]

From 1919–23, while living in France, Nguyễn Sinh Cung began to approach the idea of communism, through his friend and Socialist Party of France comrade Marcel Cachin. Cung claimed to have arrived in Paris from London in 1917, but the French police only had documents of his arrival in June 1919.^[3] Following World War I, under the name Nguyễn Ái Quốc ("Nguyễn the Patriot"), he petitioned for recognition of the civil rights of the Vietnamese people in French Indochina to the Western powers at the Versailles peace talks, but was ignored.^[5] Citing the language and the spirit of the U.S. Declaration of Independence, Quốc petitioned U.S. President Woodrow Wilson to help remove the French from Vietnam and replace them with a new, nationalist government. Although he was unable to obtain consideration at Versailles, the failure further radicalized Nguyễn, while also making him a national hero of the anti-colonial movement at home in Vietnam.^[6]

In 1920, during the Congress of Tours, in France, Quốc became a founding member of the Parti Communiste Français (FCP) and spent much of his time in Moscow afterward, becoming the Comintern's Asia hand and the principal theorist on colonial warfare. During the Indochina War, the PCF would be involved with anti-war propaganda, sabotage and support for the revolutionary effort. In May 1922, Nguyễn wrote an article for a French magazine criticizing the use of English words by French sportswriters.^[7] The article implores Prime Minister Raymond Poincaré to outlaw such Franglais as le manager, le round and le knock-out. While living in Paris, he reportedly had a relationship with a dressmaker named Marie Brière.^[7]

In the Soviet Union and China[link]

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In 1923, Nguyễn (Hồ) left Paris for Moscow, where he was employed by the Comintern, studied at the Communist University of the Toilers of the East,^[8][9] and participated in the Fifth Comintern Congress in June 1924, before arriving in Canton (present-day Guangzhou), China, in November 1924. In June 1925, Hoàng Văn Chí claimed Nguyễn (Hồ) had betrayed Phan Bội Châu, the head of a rival revolutionary faction, to French police in Shanghai for 100,000 piastres.^[10] Nguyễn (Hồ) later claimed he did it because he expected Châu's trial to stir up anti-French resentment, and because he needed the money to establish a communist organization.^[10] In Ho Chi Minh: A Life, William Duiker repudiated this hypothesis. Other sources claim that Nguyễn Thượng Hiền was responsible for Châu's capture. Châu never denounced Nguyễn.

In 1925-26 he organized "Youth Education Classes" and occasionally gave lectures at the Whampoa Military Academy on the revolutionary movement in Indochina. According to Duiker, he lived with and married a Chinese woman, Tăng Tuyết Minh (née Zeng Xueming), on 18 October 1926.^[11] When his comrades objected to the match, he told them, “I will get married despite your disapproval because I need a woman to teach me the language and keep house.”^[11] She was 21 and he was 36.^[11] They married in the same place where Zhou Enlai had married earlier and then lived together at the residence of a Comintern agent, Mikhail Borodin.^[11]

Chiang Kai-shek's anti-communist 1927 coup triggered a new round of exile for Nguyễn. He left Canton again in April 1927 and returned to Moscow, spending some of the summer of 1927 recuperating from tuberculosis in the Crimea, before returning to Paris once more in November. He then returned to Asia by way of Brussels, Berlin, Switzerland, and Italy, from where he sailed to Bangkok, Thailand, where he arrived in July 1928. “Although we have been separated for almost a year, our feelings for each other do not have to be said in order to be felt”, he reassured Minh in an intercepted letter.^[11]

He remained in Thailand, staying in the Thai village of Nachok,^[12] until late 1929 when he moved on to India, and Shanghai. In June 1931, he was arrested in Hong Kong. To reduce French pressure for extradition, it was (falsely) announced in 1932 that Nguyễn Ái Quốc had died.^[13] The British quietly released him in January 1933. He made his way back to Milan, Italy, where he served in a restaurant. The restaurant is now a traditional Lombard-cuisine temple and harbors a portrait of Hồ Chí Minh on the wall of its main dining hall.^[14][15] He moved to the Soviet Union, where he spent several more years recovering from tuberculosis.

In 1938, he returned to China and served as an adviser with Chinese Communist armed forces, which later forced China's government to the island of Taiwan.^[3] Around 1940, Quốc began regularly using the name "Hồ Chí Minh",^[3] a Vietnamese name combining a common Vietnamese surname (Hồ, 胡) with a given name meaning "He Who enlightens" (from Sino-Vietnamese 志 明; Chí meaning 'will' (or spirit), and Minh meaning "light").^[16]

Independence movement[link]

In 1941, Hồ returned to Vietnam to lead the Việt Minh independence movement. The “men in black” were a 10,000 member guerrilla force that operated with the Việt Minh.^[17] He oversaw many successful military actions against the Vichy French and Japanese occupation of Vietnam during World War II, supported closely but clandestinely by the United States Office of Strategic Services, and later against the French bid to reoccupy the country (1946–54). He was jailed in China by Chiang Kai-shek's local authorities before being rescued by Chinese Communists.^[18] Following his release in 1943, he returned to Vietnam. He was treated for malaria and dysentery by American OSS doctors.

Following the August Revolution (1945) organized by the Việt Minh, Hồ became Chairman of the Provisional Government (Premier of the Democratic Republic of Vietnam) and issued a Proclamation of Independence of the Democratic Republic of Vietnam.^[19] Although he convinced Emperor Bảo Đại to abdicate, his government was not recognized by any country. He repeatedly petitioned American President Harry S. Truman for support for Vietnamese independence,^[20] citing the Atlantic Charter, but Truman never responded.^[21]

According to some unverified sources,^[22] 1945, in a power struggle, the Việt Minh killed members of rival groups, such as the leader of the Constitutional Party, the head of the Party for Independence, and Ngô Đình Diệm's brother, Ngô Ðình Khôi.^[23] Purges and killings of Trotskyists were also documented in The Black Book of Communism.

In 1946, when Hồ traveled outside of the country, his subordinates imprisoned 2,500 non-communist nationalists and forced 6,000 others to flee.^[24] Hundreds of political opponents were jailed or exiled in July 1946, notably members of the National Party of Vietnam and the Dai Viet National Party, after a failed attempt to raise a coup against the Vietminh government.^[25][26] All rival political parties therefore banned and local governments purged^[27] to minimize opposition later on.

However, it was noted that the Democratic Republic of Vietnam's first Congress had over two-third of its members come from non-Vietminh political factions, some without election. NPV party leader Nguyễn Hải Thần was named Vice President.^[28] They also held four out of ten ministerial positions.^[29]

Birth of the Democratic Republic of Vietnam[link]

On 2 September 1945, following Emperor Bảo Đại's abdication, Hồ Chí Minh read the Declaration of Independence of Vietnam,^[30] under the name of the Democratic Republic of Vietnam. In Saigon, with violence between rival Vietnamese factions and French forces increasing, the British commander, General Sir Douglas Gracey, declared martial law. On 24 September, the Việt Minh leaders responded with a call for a general strike.^[31]

In September 1945, a force of 200,000 Republic of China Army troops arrived in Hanoi. Hồ made a compromise with their general, Lu Han, to dissolve the Communist Party and to hold an election which would yield a coalition government. When Chiang later traded Chinese influence in Vietnam for French concessions in Shanghai, Hồ Chí Minh had no choice but to sign an agreement with France on 6 March 1946, in which Vietnam would be recognized as an autonomous state in the Indochinese Federation and the French Union. The agreement soon broke down. The purpose of the agreement, for both the French and Vietminh was to drive out Chiang's army from North Vietnam. Fighting broke out in the North soon after the Chinese left.

“The last time the Chinese came, they stayed a thousand years. The French are foreigners. They are weak. Colonialism is dying. The white man is finished in Asia. But if the Chinese stay now, they will never go. As for me, I prefer to sniff French shit for five years than to eat Chinese shit for the rest of my life.” — Hồ Chí Minh, 1946^[32]

The Viet Minh then collaborated with French colonial forces to massacre supporters of the Vietnamese nationalist movements in 1945-6.^[33] The Communists eventually suppressed all non-Communist parties but failed to secure a peace deal with France. In the final days of 1946, after a year of diplomatic failure and many concessions in agreements such as the Dalat and Fontainebleau conferences, the Democratic Republic of Vietnam government found that war was inevitable. The bombardment of Haiphong by French forces at Hanoi only strengthened the belief that France had no intention of allowing an autonomous, independent state in Vietnam. On 19 December 1946, Hồ, representing his government, declared war against the French Union, marked the beginning of the Indochina War.^[34] The Vietnam National Army, by then mostly armed with machetes and muskets immediately attacked, waging assault against French positions, smoking them out with straw bundled with chili pepper, destroying armored vehicles by Lunge Mines and Molotov cocktails, holding off attackers by using roadblocks, mines and gravel. After two month of fighting, the exhausted Việt Minh forces withdrew after systematically destroying any valuable infrastructure. Hồ was reported to be captured by a group of French soldiers led by Jean-Etienne Valluy at Việt Bắc in Operation Lea which turned out to be a Việt Minh advisor, who was later killed trying to escape. According to journalist Bernard Fall, after fighting the French for several years, Hồ decided to negotiate a truce. The French negotiators arrived at the meeting site: a mud hut with a thatched roof. Inside they found a long table with chairs and were surprised to discover in one corner of the room a silver ice bucket containing ice and a bottle of good Champagne which should have indicated that Hồ expected the negotiations to succeed. One demand by the French was the return to French custody of a number of Japanese military officers (who had been helping the Vietnamese armed forces by training them in the use of weapons of Japanese origin), in order for them to stand trial for war crimes committed during World War II. Hồ replied that the Japanese officers were allies and friends whom he could not betray. Then he walked out, to seven more years of war.^[35]

In February 1950, after the successful removal of French border's blockade,^[36] Hồ met with Stalin and Mao Zedong in Moscow after the Soviet Union recognized his government. They all agreed that China would be responsible for backing the Việt Minh.^[37] Mao's emissary to Moscow stated in August that China planned to train 60-70,000 Việt Minh in the near future.^[38] The road to the outside world was open for Việt Minh forces to receive additional supplies which allow them to escalate the fight against the French regime throughout Indochina. In 1954, after the crushing defeat of French Union forces at Điện Biên Phủ, France was forced to give up its fight against the Viet Minh.

Becoming president[link]

Hồ Chí Minh (right) with Võ Nguyên Giáp (left) in Hanoi, 1945

Hồ Chí Minh with East German sailors in Stralsund harbour, 1957

House of “Uncle Hồ” in Hanoi

The 1954 Geneva Accords, concluded between France and the Việt Minh, provided Vietminh forces would regroup in the North and the French and their colonial army (which was later known as the Army of Republic of Vietnam) forces regroup in the South. Hồ's Democratic Republic of Vietnam relocated to Hanoi and became the government of North Vietnam, a communist-led single party state. The Geneva accords also provided for a national election to reunify the country in 1956, but this was rejected by Diệm's government and the United States.^[39] The U.S government committed itself to contain the spread of communism in Asia beginning in 1950, when they funded 80% of the French effort. After Geneva, the U.S became the replacement for France as Republic of Vietnam's chief sponsor and financial backer, but there was never a written treaty between the United States and South Vietnam.^{[citation needed]}

Following the Geneva Accords, there was to be a 300-day period in which people could freely move between the two regions of Vietnam, later known as South Vietnam and North Vietnam. Some 900,000 to 1 million Vietnamese, mostly Catholics, as well as many anti-communist intellectuals, former French colonial civil servants and wealthy Vietnamese, left for the South, while around 250,000 people, mostly Vietminh soldiers, went from South to North.^[40][41] Some Canadian observers claimed many were forced by North Vietnamese authorities to remain against their will.^[42] With the backing of the U.S., the 1956 elections were canceled by Diệm, Vietnam's premier, and later the first president of Republic of Vietnam. Diệm formed another election, which he won by fraud.^[43]

In North Vietnam Political opposition groups were suppressed; those publicly opposing the government were imprisoned in hard labor camps. Prisoners were abused and beaten atop of labor-intensive work forced upon them. Many died of exhaustion, starvation, illness (who often died without any medical attention), or assault by prison guards. Up to an estimated 172,000 North Vietnamese died under the mass slaughter of "landlords" during land reform. Torture was used on a wide scale, so much so that by 1954 Ho Chi Minh became concerned, and had it banned.^[44] Dr. Steven Rosefielde, professor of economics at the University of North Carolina, places an estimated death toll at between 200,000 to 900,000. ^[45]

At the end of 1959, Lê Duẩn was appointed acting party leader, after knowing the election would never happened and Diệm's intention to purge out all opposing forces (mostly ex-Việt Minh), began request the Politburo to sending aid to the Vietcong newly uprising in South Vietnam. This was considered by Western's analyzers as a loss of power by Hồ, who is said to have preferred the more moderate Giáp for the position.^[46] The Hồ Chí Minh Trail was established in late 1959 to allow aid to be sent to the Vietcong through Laos and Cambodia, thus escalating the war and tipping the balance, turning it to their favor.^[47] Duẩn was officially named party leader in 1960, leaving Hồ a public figure for Vietnamese rather than actually governing the country. Hồ maintained much influence in the government, Tố Hữu, Lê Duẩn, Trường Chinh, and Phạm Văn Đồng would often share dinner with him, and later all of them remained key figures of Vietnam throughout and after the war. In 1963, Hồ purportedly corresponded with South Vietnamese President Diệm in the hopes of achieving a negotiated peace.^[48] This correspondence was a factor in the U.S. decision to tacitly support a coup against Diệm later that year.^[48]

In late 1964, PAVN combat troops were sent southwest into neutral Laos and Cambodia.^[49] According to Chen Jian, during the mid-to-late 1960s, Lê Duẩn permitted 320,000 Chinese volunteers into North Vietnam to help build infrastructure for the country, thereby freeing a similar number of PAVN personnel to go south.^[50] However, there is no sources from Vietnam, US or Soviet confirmed about the number of Chinese troops stationed in Northern Vietnam. By early 1965, U.S. combat troops began arriving in South Vietnam, first to protect the airbases around Chu Lai and Danang, later to take on most of the fight, as "More and more American troops were put in to replace Saigon troops who could not, or would not, get involved in the fighting".^[51]

As the "quick victory" promises failed and fighting escalated, widespread bombing all over Vietnam by the U.S. Air Force and Navy escalated Operation Rolling Thunder. Hồ remained in Hanoi during his final years, demanding the unconditional withdrawal of all foreign troops in Southern Vietnam. By July 1967, Hồ and most of the Politburo of Workers Party of Vietnam concluded the war had fallen into a stalemate, since the United States Army presence forced the People's Army of Vietnam to expend the majority of their resources maintaining the Hochiminh Trail instead of reinforcing their comrade's ranks in the South. With Hồ's permission, the Vietcong planned to execute the Tet Offensive, gambling on taking the South by force and defeating the U.S. military. The offensive came at great cost and with heavy casualties on NLF's political branches and armed forces but achieving a fundamental change in the attitudes of people in the South. Up until Tet, many civilians generally favored the Vietcong; in the wake of mass executions and looting at Hue, popular support evaporated away from the Vietcong.^[52] It appeared to Hồ and to the rest of his government that the scope of the action had shocked the public on a global scale, that up until then had been assured just before Tet that the Communists were "on the ropes". The overly positive spin that the U.S. military had been attempting to achieve for years came crashing down. The bombing of Northern Vietnam and Ho Chi Minh trail was halted, and U.S and Vietnamese negotiators began to discuss how to end the war.

From then on, Hồ and his government realized that instead of trying to face the might of the U.S. Army, which would ultimately wear them down, merely prolonging the conflict would lead to eventual acceptance of Hanoi's terms. By 1969, with negotiations still dragging on, Hồ's health began to deteriorate from multiple health problems, including diabetes which prevented him from participating in further active politics. However, he insisted that his forces in the south continue fighting until all of Vietnam was reunited under his government regardless of the length of time that it might take, believing that time and politics were on his side.^{[citation needed]}

Death[link]

Hồ Chí Minh mausoleum, Hanoi

Hồ Chí Minh statue outside Hồ Chí Minh City Hall, Hồ Chí Minh City

With the outcome of the Vietnam War still in question, Hồ Chí Minh died at 9:47 a.m. on the morning of 2 September 1969 from heart failure at his home in Hanoi, aged 79. His embalmed body is currently on display in a mausoleum in Ba Dinh Square in Hanoi despite his will requesting that he be cremated.^[53] News of his death was withheld from the North Vietnamese public for nearly 48 hours due to it being the anniversary of the founding of the Democratic Republic of Vietnam. He was not initially replaced as president, but a "collective leadership" composed of several ministers and military leaders took over, known as the Politburo. Six years after his death, after the Fall of Saigon, several PAVN tanks in Saigon displayed a poster with the quote: "You are always marching with us, Uncle Hồ". In the campaign, there was a famous song written by Huy Thuc, often sung by People's Army of Vietnam soldiers along the trail of the offensive, "Bác vẫn cùng chúng cháu hành quân" ("You are always marching with us, Uncle Ho").^[54]

Legacy[link]

Ho Chi Minh, Elizabeth Aubrac, and Lucie Aubrac in 1946

The former capital of South Vietnam, Saigon, was officially renamed Hồ Chí Minh City on 1 May 1975 shortly after its capture which officially ended the war.

Hồ's embalmed body is on display in Hanoi in a granite mausoleum modeled after Lenin's Tomb in Moscow. Streams of people queue each day, sometimes for hours, to pass his body in silence. This is similar to other Communist leaders like Vladimir Lenin and Mao Zedong.

The Hồ Chí Minh Museum in Hanoi is dedicated to his life and work.

Chilean musician Victor Jara references Hồ Chí Minh in his song "El Derecho de Vivir en Paz" ("The Right to Live in Peace").

In Vietnam today, Hồ's image appears on the front of Vietnamese currency notes. His portrait and bust are featured prominently in many of Vietnam's public buildings, classrooms (both public and private schools) and in many families' altars. There's at least one temple dedicated to him, built in Vinh Long in 1970, shortly after his death right in the heart of Republic of Vietnam control areas.^[55]

In 1987, UNESCO officially recommended to member states that they "join in the commemoration of the centenary of the birth of President Hồ Chí Minh by organizing various events as a tribute to his memory", considering "the important and many-sided contribution of President Ho Chi Minh in the fields of culture, education and the arts" who "devoted his whole life to the national liberation of the Vietnamese people, contributing to the common struggle of peoples for peace, national independence, democracy and social progress."^[56]

Publications about Hồ's non-celibacy are banned in Vietnam. A newspaper editor in Vietnam was dismissed from her post in 1991 for publishing a story about Tăng Tuyết Minh.^[57][58] William Duiker's Ho Chi Minh: A Life (2000) presents much information on Hồ's relationships.^[59] The government requested substantial cuts in the official Vietnamese translation of Duiker's book, which was refused.^[60] In 2002, the Vietnamese government suppressed a review of Duiker's book in the Far Eastern Economic Review.^[60]

References[link]

Further reading[link]

Essays[link]

• Bernard B. Fall, ed., 1967. Ho Chi Minh on Revolution and War, Selected Writings 1920-1966. New American Library.

Biography[link]

• William J. Duiker. 2000. Ho Chi Minh: A Life. Theia.
• Jean Lacouture. 1968. Ho Chi Minh: A Political Biography. Random House.
• Khắc Huyên. 1971. Vision Accomplished? The Enigma of Ho Chi Minh. The Macmillan Company.
• David Halberstam. 1971. Ho. Rowman & Littlefield.
• Hồ chí Minh toàn tập. NXB chính trị quốc gia
• Sophie Quinn-Judge. 2003. Ho Chi Minh: The missing years. C. Hurst & Co. ISBN 1-85065-658-4
• Ton That Thien, Was Ho Chi Minh a Nationalist? Ho Chi Minh and the Comintern Information and Resource Centre, Singapore, 1990

The Việt Minh, NLF and the Democratic Republic of Vietnam[link]

• William J. Duiker. 1981. The Communist Road to Power in Vietnam. Westview Press.
• Hoang Van Chi. 1964. From colonialism to communism. Praeger.
• Truong Nhu Tang. 1986. A Viet Cong Memoir. Vintage.

The War in Vietnam[link]

• Frances FitzGerald. 1972. Fire in the Lake: The Vietnamese and the Americans in Vietnam. Little, Brown and Company.

American foreign policy[link]

• Christopher Hitchens. 2001. The Trial of Henry Kissinger. Verso.
• Henry A. Kissinger. 1979. White House Years. Little, Brown.
• Richard Nixon. 1987. No More Vietnams. Arbor House Pub Co.

External links[link]

	Vietnam portal
	Biography portal

Wikisource has original works written by or about: Ho Chi Minh

Wikiquote has a collection of quotations related to: Ho Chi Minh

Wikimedia Commons has media related to: Ho Chi Minh

• The Drayton Court Hotel
• Hồ Chí Minh obituary, The New York Times, 4 September 1969
• TIME 100: Hồ Chí Minh
• Hồ Chí Minh's biography
• Satellite photo of the mausoleum on Google Maps
• [8]
• Final Tribute to Hồ from the Central Committee of the Vietnam Workers' Party
• Bibliography: Writings by and about Hồ Chí Minh
• Booknotes interview with William Duiker on Hồ Chí Minh: A Life, November 12, 2000

v t e Vietnamese independence movement Events Bombardment of Tourane Capture of Saigon Capture of the Citadel of Saigon Conquest of Cochinchina Ba Dinh uprising Pacification of Tonkin Hanoi Poison Plot World War I 1916 Cochinchina uprising Thai Nguyen uprising Bazin assassination Yen Bai mutiny World War II Second French Indochina Campaign August Revolution Proclamation of Independence of the Democratic Republic of Vietnam First Indochina War Battle of Dien Bien Phu Geneva Conference Organisations Can Vuong Dong Du Duy Tan Hoi Empire of Vietnam Nguyen dynasty Tonkin Free School Viet Nam Quang Phuc Hoi Viet Nam Quoc Dan Dang Viet Minh Vietnam Communist Party Vietnamese revolutionaries Cuong De Dinh Cong Trang Ho Chi Minh Huynh Thuc Khang Luong Van Can Ngo Dinh Diem Ngo Duc Ke Nguyen An Ninh Nguyen Dinh Chieu Nguyen Quang Bich Nguyen Quyen Nguyen Thai Hoc Nguyen Than Hien Nguyen Thanh Nguyen Thien Thuat Nguyen Thuong Hien Nguyen Trung Truc Nguyen Xuan On Pham Banh Phan Boi Chau Phan Chu Trinh Phan Dinh Phung Phan Thanh Gian Phan Xich Long Ta Thu Thau Ton That Thuyet Tran Cao Van Tran Trong Kim Truong Dinh Emperors Tu Duc Ham Nghi Thanh Thai Duy Tan Bao Dai French rulers Albert Sarraut Jean Decoux French Indochina Governor-General Collaborators Hoang Cao Khai Tran Ba Loc Nguyen Than

v t e Post-World War II Heads of state of Vietnam North Vietnam (1945 – 1976) Ho Chi Minh Ton Duc Thang South Vietnam (1946 – 1976) Republic of Cochinchina (1946 – 48) Nguyen Van Thinh Nguyen Van Xuan Le Van Hoach Nguyen Van Xuan Central Government (1948 – 49) Nguyen Van Xuan State of Vietnam (1949–55) Bao Dai Ngo Dinh Diem1 Republic of Vietnam (1955 – 75) Presidents Ngo Dinh Diem Duong Van Minh2 Nguyen Khanh2 Duong Van Minh2 Nguyen Khanh2 Duong Van Minh2 Phan Khac Suu2 Nguyen Van Thieu2 Tran Van Huong1, 2 Duong Van Minh1, 2 PRG (1975 – 76) Huynh Tan Phat Vietnam (1976 – ) Ton Duc Thang Nguyen Huu Tho1 Truong Chinh Vo Chi Cong Le Duc Anh Tran Duc Luong Nguyen Minh Triet Truong Tan Sang 1acting 2military