Figure 1. Young rivers (A) close to their source tend to be fast-flowing, high-energy environments with rapid downward and headward erosion, despite the hardness of the rock over which they may flow. Steep-sided "V-shaped' valleys, waterfalls, and rapids are characteristic features. Mature rivers (B) are lower-energy systems. Erosion takes place on the outside of bends, creating looping meanders (1) in the soft alluvium of the river plain. Deposition occurs on the inside of bends and on the river bed. At a river's mouth (C), sediment is deposited as the velocity of the river slows. As the river becomes shallower more deposition occurs, forming islands and braiding the main channel into multiple, narrower channels. As the sediment is laid down (2), the actual mouth of the river moves away from the source into the sea or lake, forming a delta.
Figure 2. At its delta at the Mediterranean Sea, the Nile broadens into a large fan-shaped alluvial plain. Credit: NASA.
Figure 3. Large alluvial fan in the Taklimakan Desert, Xinjiang Province, China. Image source: USGS Landsat Project.
Figure 4. Lisbon, the capital of Portugal, is observable north of the Tagus River estuary in this photo taken from the Space Shuttle. The estuary of the Tagus River, the longest river in the Iberian Peninsula, is 19 km long and is considered one of the best harbors in Europe. Visible south of the Tagus River estuary are the cites of Almada, Barreiro, and Montijo; farther south are Setúbal Bay and the Sado River estuary.
Figure 5. The Firth of Forth, near Edinburgh.
Figure 6. A meandering river.
Figure 7. Oxbow lakes are formed when the neck of a looping meander is broken through (A), usually during times of flood. The entrances to the bypassed meander are soon blocked by silt (B).
Figure 8. Process of change at work within a river. The material of the river-bed is being continually worn away, and transported and deposited elsewhere; how much and how far depends on the river's speed and turbulence. The movement of eroded material is indicated by arrows. (1) Straight river with symmetrical bed; the eroded material is deposited on the banks when the water level is high. (2) Winding river with an asymmetrical bed; material is worn off the concave bank, usually the outer side of a curve, and deposited on the convex.
A river is a body of inland water that flows downhill under gravity in a natural channel into the sea, a lake, or, as a tributary, into another river. The main sources of rivers are springs, lakes, and glaciers. Near the source a river flows swiftly, the rocks and other abrasive particles eroding a steep-sided V-shaped valley (see erosion). Variations in the hardness of the rocks over which it runs may result in waterfalls. In the middle part of its course the gradients become less steep, and lateral (sideways) erosion becomes more important than downcutting. The valley is broader, the flow less swift, and meandering more common. Toward the river mouth, the flow becomes more sluggish and meandering prominent: the river may form oxbow lakes. Sediment may be deposited to form a delta(see Figure 1).
Features of rivers
A delta is a flat alluvial plain at a river mouth or at the confluence of two rivers, formed of fertile mud deposited by the slowing-moving water (see Figure 2). Typically, the stream divides and subdivides until a fan-shaped plain, called an alluvial fan, covered by a complex of channels results. The form of a delta depends of the rates of sedimentation and of erosion by the sea.
An alluvial fan is a generally fan-shaped area of alluvium (water-borne sediment) deposited by a river when it reaches a plain on lower ground, and the speed of flow of the water is abruptly reduced (see Figure 3).
Sand, gravel, and silt are the main constituents of the alluvium, with the coarser material deposited near the head of the fan. Organic matter is also transported, making the soil highly fertile. Valuable minerals such as cassiterite (tin ore, SnO2), diamonds, gold, and platinum are often found in alluvial fans.
An estuary is the typically funnel-shaped part of a river near its mouth where fresh- and seawater mix and which is affected by the tides (see Figure 4). At ebb tide both tide and river current assist in the erosion of the estuary. Estuaries may also form by local subsidence of the coast. As well as the mouths of rivers, estuaries may include bays, salt marshes, and lagoons. These brackish water ecosystems shelter and feed marine life, birds, and wildlife, but are particularly vulnerable to damage as a result of human actions. Many estuaries provide important harbors.
"Firth" is a term used primarily in Scotland to describe usually a long narrow estuary, often a fjord, and sometimes a strait. The best known are those of the Forth (see Figure 5), Tay, and Clyde; the Solway Firth, into which several rivers drain; the Moray Firth, between the northeast tip of Loch Ness and the North Sea; and the Pentland Firth, the strait between northeast Scotland and the Orkney Islands.
A meander is a naturally-occurring loop-like bend in the course of a river will wind round any obstacle, such as hard rock (see Figure 6). Once a meander has been created it will continue, becoming accentuated by the erosive action of the river. On the outside of a bend there will be lateral corrasion, which will gradually work out sideways. On the inside of the bend there is likely to be some deposition, which will build up a flat flood plain. Meanders gradually move downstream. Sometimes they make complete loops, which when cut off, form oxbow lakes. The name comes from the winding River Maeander in Asian Turkey.
An oxbow lake is a crescent-shaped section of a river channel that no longer carries the main discharge of water (see Figure 7). An oxbow lake forms from a meander. As sediment is deposited, the meander becomes cut off from the river to create a lake. Once formed, the lake gradually shrinks as silt fills it in; vegetation grows on the new muddy area, and the land can be reclaimed. The name derives from the shape of the lake, said to resemble an ox's collar.
Discharge and speed of a river
The discharge of a river is the volume of water flowing past a point in a given time. It is usually expressed as cubic meters per second (cumecs), and is calculated by multiplying the cross-sectional area of the river by the speed of the water. The speed of a river is controlled by the slope of the river, the depth of the river and the roughness of the river bed.
Rivers transport sediment as they flow, by the process of traction (rolling), saltation (jumping), suspension (carrying). and solution. A greater discharge increases the amount of sediment that can be transported during flood conditions, but as a river returns to normal flow it deposits sediment. A river adjusts its channel shape to be able to transport sediment most efficiently (see Figure 8). This can result in the erosion of a river channel or the building up of floodplains, and sand and gravel banks.
Rivers flood when their channels cannot contain the discharge. Flood risk can be reduced by straightening the channel, dredging sediment or making the channel deeper by raising the banks.
Water gaps and wind gaps
A water gap is a short, narrow gorge cut through a ridge or region of high ground by a stream or river. If the river no longer passes through it, the gorge is termed a wind gap.