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Origins of river waterA 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 come 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. Image:ReichenbachBegin2.jpg The beginning of a mountain river (Reichenbach in Grosse Scheidegg)
Image:Tambo river.jpg A youthful river flowing over a slight change in topography 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. TopographyThe 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.
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.
Other types of riversMost 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.
Use of riversImage:Hooghly River 01.jpg Man has been using rivers for navigation used since the dawn of civilization. River provides 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 defences, as a source of power to drive machinery, and as a means of disposing of waste. For thousands of years rivers has been used for navigation (The earliest evidence of navigation is found in the Indus Valley Civilization, which existed in Northwestern India around 3300 BC). Riverine navigation provides the cheapest means of transport and is still used extensively in major rivers of the world like Ganges River, River Nile, Mississippi River, River Indus, etc. In some places in the world like Scandinavia, Canada, the lumberjacks uses the river to float down the logs cut by them, down to the lumber camps (which are present downstream). This natural transportation saves them the entire effort to carry the huge heavy logs to the lumber camps. River has been a source for food since the dawn of civilization. Apart from being a rich source of fish, rivers indirectly aids cultivation with its supply of water for the crops. Rivers sustains its own food chain. They are a major source of fresh water. Hence, no doubt we find most of the major cities of the world is situated on the banks of rivers. Rivers also provides a easy means of disposing of waste. 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). Fast flowing rivers and waterfalls are harnessed as sources of energy, via watermills and hydroelectric plants. Rivers have been important historically in determining political boundaries and defenses of 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 River 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.) BiologyThe 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. FloodingFlooding 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 flowA misconception, particularly amongst schoolchildren, [1][2] is that most, or even all, rivers flow from north to south. Some attribute this "fact" to such causes as the rotation of the Earth, centrifugal force, angular momentum, and the local geography effects. Rivers in fact flow downhill irrespective of direction, often in a complex meandering path involving all directions of the compass.[3][4][5] Indeed, 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, Lena, etc. Four of the ten longest river systems of the world flow mainly north. Studying the flows of rivers is one aspect of hydrology.[6] ManagementRivers 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. River listsThe world's ten longest riversIt 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.
For a longer list see Longest rivers. This also gives more information on measuring river lengths. Well-known rivers (in alphabetic order)
Other listsRivers in myth and fictionReal rivers
Mythological or Fictional rivers
Rating systems
References
Further reading
See alsoCrossingsRivers may be crossed by: Transport
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