River

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This bridge across the Danube River links Hungary with Slovakia.

A river is a natural waterway that transits water through a landscape from higher to lower elevations. It is an integral component of the water cycle. The water within a river is generally from precipitation through surface runoff, groundwater recharge (as seen at baseflow conditions / during periods of lack of precipitation) and release of stored water in natural reservoirs, such as a glacier.

Contents

  • 1 Origins of river water
  • 2 Topography
  • 3 Other types of rivers
  • 4 Use of rivers
  • 5 Biology
  • 6 Flooding
  • 7 Direction of flow
  • 8 Rate of water flow
  • 9 Management
  • 10 River lists
    • 10.1 The world's ten longest rivers
    • 10.2 Well-known rivers (in alphabetic order)
    • 10.3 Other lists
  • 11 Rating systems
  • 12 See also
    • 12.1 Crossings
    • 12.2 Transport
  • 13 References
  • 14 Further reading

[edit] Origins of river water

A youthful river flowing over a slight change in topography
The beginning of a mountain river (Reichenbach in Grosse Scheidegg)

A river may have its source in a spring, lake, from damp, boggy landscapes where the soil is waterlogged, from glacial melt, or from surface runoff of precipitation. Almost all rivers are joined by other rivers and streams termed tributaries the highest of which are known as headwaters. Water may also originate from groundwater sources. Throughout the course of the river, the total volume 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.

From their source, all rivers flow downhill, typically terminating in the sea or in a lake, through a confluence. In arid areas rivers sometimes end by losing water to evaporation. River water may also infiltrate into the soil or pervious rock, where it becomes groundwater. Excessive abstraction of water for use in industry, irrigation, etc., can also cause a river to dry before reaching its natural terminus.

The mouth, or lower end, of a river is known by hydrologists as its base level.

The area drained by a river and its tributaries is called catchment, catchment basin, drainage basin or watershed. The term "watershed" is also used to mean a boundary between catchments, which is also called a water divide, or in some cases, continental divide.

[edit] Topography

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 flood-plain 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 flood-plain can be blurred especially in urban areas where the flood-plain of a river channel can become greatly developed by housing and industry.

The river channel itself 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 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.

A river flowing in its channel is a source of considerable energy which acts on the river channel to change its shape and form. 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, loops (meanders) may form through eroding 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. River mouths may also be fjords or rias.

Although the following classes are a useful simplified way to visualize rivers, it is important to recognize there are other factors at work here. Gradient is controlled largely by tectonics, but discharge is controlled largely by climate and sediment load is controlled by various factors including climate, geology in the headwaters, and the stream gradient.

It has been noted that on average, the air distance from the beginning to the end of most rivers is about one third their actual length. For rivers that flow in plain areas, this number is very close to Pi; Einstein wrote an explanation of why this is so.[1][2]

[edit] Other types of rivers

Most rivers flow on the surface, however other rivers may flow underground in caves or caverns. Such rivers can be found in karst regions with limestone geologic formations.

An intermittent river (or ephemeral river) flows occasionally and can be dry for several years at a time. These rivers are found in regions with limited and highly variable rainfall.

[edit] Use of rivers

Man has been using rivers for navigation since the dawn of civilization. Rivers provide the cheapest means of transport. In this figure a country boat is seen plying over Hooghly River at Kolkata, India.

Rivers have been used by man since the dawn of civilization as a source of water, for food, for transport, as a defensive barrier, as a source of power to drive machinery, and as a means of disposing of waste.

For thousands of years rivers have been used for navigation (The earliest evidence of navigation is found in the Indus Valley Civilization, which existed in north-western India around 3300 BC). Riverine navigation provides the cheapest means of transport and is still used extensively on major rivers of the world like the Ganges, the Nile, the Mississippi, and the Indus.

In some highly-forested countries like 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. Apart from being a rich source of fish, rivers indirectly aid cultivation by supplying water for the crops. Rivers sustain their own food chain. They are a major source of fresh water, hence, it is no surprise to find most of the major cities of the world situated on the banks of rivers. Rivers also provide an easy (if unsanitary) means of disposing of waste.

Most riverbanks in Japan are used as places for playing, recreation and parties

The rocks and gravel generated and moved by rivers have been greatly used in construction. In more recent generations, the beauty of rivers and their wider habitats has contributed greatly to tourist income from areas well endowed with attractive riverine scenery.

In upland rivers, rapids with whitewater or even waterfalls occur. Rapids are often used for recreational purposes (see whitewater kayaking). Fast flowing rivers and waterfalls are harnessed as sources of energy, via watermills and hydroelectric plants.

The Amazon River near Manaus in Brazil.

Rivers have been important historically in determining political boundaries and defending countries. For example, the Danube was a longstanding border of the Roman Empire, and today 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 various provinces and countries along their routes.

The noted Greek historian Megasthenes (350BC-290BC) mentions about River Ganga several times in his work Indika: "India, again, possesses many rivers both large and navigable, which, having their sources in the mountains which stretch along the northern frontier, traverse the level country, and not a few of these, after uniting with each other, fall into the river called the Ganges. Now this river, which at its source is 30 stadia broad, flows from north to south, and empties its waters into the ocean forming the eastern boundary of the Gangaridai, a nation which possesses a vast force of the largest-sized elephants." (Diodorus II.37.)

[edit] Biology

Main article: Aquatic ecosystem

The flora and fauna of rivers have developed to utilise the very wide range of aquatic habitats available from torrential waterfalls through to lowland mires. Although many organisms are restricted to the fresh-water in rivers, some, such as Salmon and Hilsa have adapted to be able to survive both in rivers and in the sea.

[edit] Flooding

Main article: Flood

Flooding is a natural part of a river's cycles. The majority of the erosion of river channels and the erosion and deposition on the associated floodplains occur during flood stage. Human activity, however, has upset the natural way flooding occurs by walling off rivers, straightening their courses and by draining of natural wetlands.

Flooding can be mitigated.

[edit] Direction of flow

A misconception, is that most, or even all, rivers flow from north to south.[3][4] Rivers in fact flow down gradient irrespective of direction, often in a complex meandering path involving all directions of the compass.[5][6][7]

As it happens, few major rivers in the continental US flow north, as most of the country is located in the watershed of the Pacific or Atlantic oceans or the Gulf of Mexico, with very few rivers flowing northward toward the Arctic Ocean, Great Lakes, or Hudson Bay. However, thousands of north-flowing rivers exist elsewhere, including such major watercourses as the Nile, Mackenzie, Rhine, Yenisei, Nelson, and Lena. Four of the ten longest river systems of the world flow mainly north.

Studying the flows of rivers is one aspect of hydrology.[8]

[edit] Rate of water flow

Volumetric flow rate, also called volume flow rate and rate of water flow, is the volume of water which passes through a given volume per unit time, measured in cubic meters per second ( 1 m3/s = 35.31 ft3/s).

[edit] Management

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

River management is an ongoing activity as rivers tend to 'undo' the modifications made by man. 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 effects of such management. As an example, in many parts of the developed world, rivers have been confined within channels to free up flat flood-plain land for development. Subsequent extreme flood events can inundate such development at very high financial costs and often with loss of life.

[edit] River lists

[edit] The world's ten longest rivers

Because rivers are approximately fractal in nature it is difficult to measure the length of a river. The more precise the measurement, the longer the river will seem. Also, it is difficult to determine where a river begins or ends, as very often, upstream rivers are formed by seasonal streams, swamps, or changing lakes. These are average measurements.

  1. Nile River (6,695 km)
  2. Amazon River (6,400 km)
  3. Jefferson-Missouri-Mississippi (6,270 km)[9]
  4. Yangtze (Chang Jiang) (6,245 km)[10]
  5. Yenisey-Angara (5,550 km)
  6. Huang He (Yellow) (5,464 km)
  7. Ob-Irtysh (5,410 km)
  8. Amur (4,410 km)
  9. Congo (4,380 km)
  10. Lena (4,260 km)

For a longer list see Longest rivers. This also gives more information on measuring river lengths.

[edit] Well-known rivers (in alphabetic order)

[edit] Other lists

[edit] Rating systems