Difference between revisions of "River" - New World Encyclopedia

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Revision as of 20:22, 18 January 2007

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For other uses of the term, see River (disambiguation).
River Gambia flowing through Niokolokoba National Park

A river is a natural waterway that conveys water derived from precipitation from higher ground to lower ground. Most commonly rivers flow on the surface but there are many examples of undeground rivers where the flow is contained within chambers, caves or caverns. In some areas of highly variable rainfall, some rivers exist that carry water only occasionally and may be dry for several years at a time.

Origins of river water

Transport===

  • Barge
  • Riverboat
  • Sailing
  • Towpath

A river may have its source in a spring, lake, from damp, boggy places where the soil is waterlogged, from glacial meltwater, or simply from rain flowing off impermeable rock or man-made surfaces. Almost all rivers are joined by other rivers and streams termed tributaries the highest of which are known as headwaters. Water may also be recruited to a river from ground-water 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 underly the river and its floodplain. 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. In arid areas rivers sometimes end by losing water to evaporation. River flow may also be lost by percolation into dry, porous material such as sand, soil, or into pervious rock. Excessive abstraction of water for use in industry, irrigation etc can also cause a river to dry before reaching a lake or the sea.

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.

Topography

A river flowing over a slight change in topography
File:A21a.JPG
Bridges are a common way of crossing rivers, as seen here at the Buller River, West Coast, New Zealand

A river's water is generally 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 overtopping the channel. Flood plains may be very wide in relation to the size of the river channel. This distinction between river channel and floo-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 may contain a single stream of water but many rivers, if left unconstrained by man's activities, will create several streams of water within a channel producing a braided river. Braided rivers can still be commonly seen in South Island New Zealand and on 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 idenitified 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. 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.

  • Youthful river - a river with a steep gradient that has very few tributaries and flows quickly. Its channels erode deeper rather than wider. (Ex: Brazos River, Trinity River, Ebro River)
  • Mature river - a river with a gradient that is less steep than those of youthful rivers and flows more slowly than youthful rivers. A mature river is fed by many tributaries and has more discharge than a youthful river. Its channels erode wider rather than deeper. (Ex: Mississippi River, Ohio River, Thames River)
  • Old river - a river with a low gradient and low erosive energy. Old rivers are characterized by flood plains. (Ex: Tigris River, Euphrates River, Indus River)
  • Rejuvenated river - a river with a gradient that is raised by tectonic uplift.
The beginning of a mountain river (Reichenbach in Grosse Scheidegg)
The source, where this river comes out of the melting ice (also visible in the previous photo)


See also: geography , transvasement , water cycle , and watershed

Use of rivers

Rivers have been used by man since the dawn of civilization as a source of water, for food, for transport as defences, as a source of power to drive machinery and as a means of disposing of waste. In addition the rocks and gravels 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). Waterfalls are sometimes used as sources of energy, via watermills and hydroelectric plants.

Geopolitical boundaries

Rivers throughout history have been the source and support for civilization, and many major cities today are near a river of some sort. Rivers have been important historically in determining political boundaries. 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 River forms the boundary between various provinces and countries along its route in Africa.

Biology

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 have adapted to be able to survive both in rivers and in the sea..

Flooding

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.

Direction of flow

A misconception, particularly amongst schoolchildren and college students in North America[1][2], is that most, or even all, rivers flow from north to south. Rivers in fact flow downhill irrespective of direction and is often a complex meandering path involving all directions of the compass.[3][4][5]

Studying the flows of rivers is one aspect of hydrology.[6]

Management

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

  • Dams (see above) or weirs may be built to control the flow, store water, or extract energy.
  • Levees may be built to prevent run-off of excess river water in times of flood.
  • 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 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.

River lists

The world's ten longest rivers

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 (6,690 km)
  2. Amazon (6,452 km)
  3. Mississippi-Missouri (6,270 km)[1]
  4. Yangtze (Chang Jiang) (6,245 km)[2]
  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.

Well-known rivers (in alphabetic order)

Other lists

  • List of waterways
    • List of rivers of Oceania
      • List of rivers of New Zealand
  • List of river name etymologies

Rivers in myth and fiction

Real rivers

  • the Thames in Edward Rutherfurd's London
  • the Thames in Jerome K. Jerome's Three Men in a Boat
  • the Thames and the Congo in Joseph Conrad's Heart of Darkness
  • the Mississippi in Mark Twain's Huckleberry Finn
  • the River Liffey through Dublin in James Joyce's Finnegans Wake

Mythological or Fictional rivers

see also river deity
  • in Greek mythology, the Acheron, Cocytus, Phlegethon, Lethe and Styx (the five rivers of Hades); and the Eridanus
  • Virginia's Nancy River alleged to have had mystical healing powers
  • the Alph, an underground river imagined by various mystics and mentioned in Coleridge's poem Kubla Khan
  • Zora's River in Ocarina of Time
  • the Tamanawis River in David James Duncan's "The River Why?"
  • the Anduin in J.R.R Tolkien's The Lord Of The Rings
  • the Lifestream in Final Fantasy VII
  • the Beartooth,edda,Gaena,Jiet,Toark,Ninor,Anora,and Ramr rivers in Christopher Paolini's Eragon and Eldest

Rating systems

  • International Scale of River Difficulty - The scale is used to rate the challenges of navigation—particularly those with rapids. Class I is the easiest and Class VI is the hardest.
  • Strahler Stream Order - The Strahler Stream Order is a method to rank rivers based on the connectivity and hierarchy of contributing tributaries. Headwaters are first order while the Amazon River is twelfth order. Approximately 80 percent of the rivers and streams on Earth are of the first and second order.

References
ISBN links support NWE through referral fees

  1. Children's Misconceptions about Science. Operation Physics, American Institute of Physics (September 1998).
  2. William C. Philips (February 1991). Earth Science Misconceptions.
  3. Matt Rosenberg (2006-06-08). Do All Rivers Flow South?.
  4. Matt Rosenberg. Rivers Flowing North: Rivers Only Flow Downhill; Rivers Do Not Prefer to Flow South.
  5. Nezette Rydell (1997-03-16). Re: What determines the direction of river flow? Elevation, Topography,Gravity??. Earth Sciences.
  6. Cristi Cave. How a River Flows. Stream Biology and Ecology.

Further reading

  • Luna B. Leopold (1994). A View of the River. Harvard University Press. ISBN 0-674-93732-5.  — a non-technical primer on the geomorphology and hydraulics of water
  • Jeffrey W. Jacobs. "Rivers, Major World". Water Encyclopaedia.

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