In addition to cutting downward into the earth, rivers have a tendency to change course over time. Yet, despite this, rivers often constitute the boundaries of adjacent land when divided for sale — I have personally read countless legal descriptions that contain the language “following the course of said river.”
As the river moves through the upper course, it cuts downwards. The gradient here is steep and the river channel is narrow. Vertical erosion in this highland part of the river helps to create steep-sided V-shaped valleys, interlocking spurs, rapids, waterfalls and gorges.
Lower course river features include wide flat-bottomed valleys, floodplains and deltas. As the river moves through the upper course, it cuts downwards. The gradient here is steep and the river channel is narrow.
These are erosion, transportation and deposition. All three depend on the amount of energy there is in a river. The energy in a river causes erosion. The bed and banks can be eroded making it wider, deeper and longer. Headward erosion makes a river longer. This erosion happens near its source.
Initially, when a slight curve is already present in the river, water travels around the outer edge of the curve faster than the inner edge, because it's covering a greater distance in the same amount of time. As water moves faster, more of the sediment in it stays suspended, instead of settling to the bottom.
Human actions that can change streamflow patterns include dam building, stream diversion, pumping of shallow groundwater, and covering the landscape with impervious surfaces such as pavement and roofs. Changes in climate also can alter flow by altering timing and amount of precipitation.
A river changes shape as it flows from its source to its mouth. The shape of both the long profile (a slice through the river from source to mouth) and the cross profile (a slice across the river) changes.
The shape of rivers and streams changes through time as erosion, deposition, and transport of sediment occurs. Rivers and streams maintain a dynamic equilibrium between discharge, slope, sediment load, and sediment size (Lane 1955).
The velocity of a river is determined by many factors, including the shape of its channel, the gradient of the slope that the river moves along, the volume of water that the river carries and the amount of friction caused by rough edges within the riverbed.
EXPLANATION: Due to constant deposition of river sediments on the slower side and the vast amount of erosion that takes place on the faster side. This process keeps on continuing till the curves get sharpened, so that river cuts through the curve and forms another path and thus river changes its course.
Stream and River Erosion Streams and rivers erode and transport sediment. They erode bedrock and/or sediment in some locations and deposit sediment in other areas. Moving water, in river and streams, is one of the principal agents in eroding bedrock and sediment and in shaping landforms.
Vertical erosionVertical erosion makes a river channel deeper. This happens more in the upper stages of a river (the V of vertical erosion should help you remember the V-shaped valleys that are created in the upper stages). Lateral erosion makes a river wider.
Rivers Create New Landforms Through the processes of erosion and deposition, rivers and streams can drastically alter the Earth's surface. The kinds of features and landforms created depend on their slope, speed, and volume. The rushing water of rivers helps to carve new features into the surface of the Earth.
Climate changes such as rising temperatures, more frequent extreme storms and changes in season precipitation rates will impact lakes, rivers and streams. As air temperatures rise, so will water temperatures in freshwater systems.
This is because, as sea level rises, rivers respond by depositing more of their sediment into the channel, which raises the riverbed relative to the neighboring land, making the river unstable. Eventually, a levee breach will force the river to find a shorter and steeper path to the sea.
The character of a river's regime is influenced by a number of variable factors: the size of the river and where discharge measurements are taken along its course. the amount, seasonality and intensity of the precipitation. the temperatures, with possible meltwater and high rates of evaporation in the summer.
From its source, a river flows downhill as a small stream. Precipitation and groundwater add to the river’s flow. It is also fed by other streams, called tributaries. For instance, the Amazon River receives water from more than 1,000 tributaries.
Rivers of Asia. Asia’s longest and most important river is the Yangtze, in China. It flows from the Dangla Mountains, between Tibet and China’s Qinghai province.
A river is a large, natural stream of flowing water. Rivers are found on every continent and on nearly every kind of land. Some flow all year round. Others flow seasonally or during wet years. A river may be only kilometers long, or it may span much of a continent. The longest rivers in the world are the Nile in Africa and ...
A river’s watershed includes the river, all its tributaries, and any groundwater resources in the area. The end of a river is its mouth. Here, the river empties into another body of water—a larger river, a lake, or the ocean. Many of the largest rivers empty into the ocean.
For centuries, scientists have debated which river is longer. Measuring a river is difficult because it is hard to pinpoint its exact beginning and end. Also, the length of rivers can change as they meander, are dam med, or their deltas grow and recede.
Rivers of Australia. Much of Australia is arid, but rivers still run through it. Australia’s principal rivers are the Murray and the Darling, both in the southeastern part of the continent. The Murray flows some 2,590 kilometers (1,610 miles) from the Snowy Mountains to a lagoon on the Indian Ocean.
Great river cities include New York City, New York; Buenos Aires, Argentina; London, England; Cairo, Egypt; Kolkata, India; and Shanghai, China. In fact, rivers are usually the oldest parts of cities.
The gradient is gentler and more lateral (sideways) erosion widens the channel. The river channel has also become deeper. Meanders are typical landforms found in this stage of the river.
Stage 2. Where the river swings toward the bank lateral (sideways) erosion causes undercutting. On the opposite side of the channel where the velocity (speed of the flow of water) is lower material is deposited. Therefore the river does not get any wider.
Meanders are typical landforms found in this stage of the river. A meander is a winding curve or bend in a river. They are typically found in the middle and lower course of a river. This is because vertical erosion is replaced by a sideways form of erosion called lateral erosion, plus deposition within the floodplain.
There are several stages involved in the creation of meanders and oxbow lakes. Stage 1. In low flow conditions, straight river channels have bars of sediment on their beds. Flowing water weaves around these bars of sediment.
Meanders are perpetuated through a process called helicoidal flow. As the surface flow of water hits the outer bank it corkscrews, flows along the river bed then deposits eroded material on the inner bank. Eventually, the neck of the meander will be breached by the river creating an ox-bow lake.
River cliff - the river moves faster on the outside of the bend and cuts into the valley side. The erosion undercuts the ground causing it to collapse, leaving a cliff. River beach - (slip-off slope) the river moves more slowly on the inside of the bend.
Source - the point at which the river starts. Interlocking spurs - where the river winds between ridges. Gorge - a deep valley caused by the wearing back of a waterfall. Waterfall - often occur where the river crosses a band of harder rock.
Gorge - a deep valley caused by the wearing back of a waterfall. Waterfall - often occur where the river crosses a band of harder rock. V-shaped valley - produced in the upper course because the river cuts down faster than the surrounding slopes are eroded.
When a river floods more substantial material and the majority of deposition occurs next to the river channel as the result of increased friction (with the flood plain ). The velocity of the river slows and therefore rapidly reduce its ability to transport material. This leaves a ridge of higher material next to the river channel on both banks of the river known as a levee.
The volume of water in a river is at its greatest in the lower course. This is due to the contribution of water from tributaries. The river channel is deep and wide and the land around the river is flat. Energy in the river is at its lowest and deposition occurs.
Rivers flood on a regular basis. The area over which they flood is known as the floodplain, and this often coincides with regions where meanders form. Meanders support the formation of floodplains through lateral (sideways) erosion. When rivers flood the velocity of water slows.
Estuary . An estuary is a wide, sheltered body of water found at a river’s mouth where it broadens into the sea. It is a combination of salt water from the sea and fresh water from a river. As the river meets the sea at high tide, it slows the flow of water leading to deposition. Mudflats and saltmarsh form in these areas.
Rapids. Rapids are sections of a river where the gradient of the river bed is relatively steep resulting in an increase in the river’s turbulence and velocity. They form where the gradient of the river is steep and the bed is composed mainly of hard rocks. Meanders.
When the rock type of the river’s channel changes from a resistant rock to a less resistant one (e.g. granite to limestone), the river erodes the less resistant rock faster producing a sudden drop in the gradient of the river with the resistant rock being higher up than the less resistant rock.
The width of a floodplain is determined by the sinuosity of the river and how much meander migration takes place. If there’s a lot of meander migration, the area that the river floods on will change and the floodplain will become wider. Levees. Levees are natural embankments produced, ironically, when a river floods.
Levees aren’t permanent structures. Once the river’s discharge exceeds its bankfull discharge1, the levees can be burst by the high pressure of the water.
Meanders. Meanders are bends in a river that form as a river’s sinuosity increases. The sinuosity of a river is a measurement of how much a river varies from a straight line. It’s a ratio between the channel length and displacement (straight line distance) between two points in the river’s course:
These currents erode the river’s bed and create small depressions in it. The creation of eddie currents as a result of bedload in a river. As these depressions deepen, pebbles can become trapped in them. As a result of the eddie currents, the pebbles drill into the depressions making them more circular, wider & deeper.
In the upper course of a river, its load is large and mainly transported by traction along the river bed. When flowing water encounters bedload, it is forced over it and downcuts behind the bedload in swirling eddie currents. These currents erode the river’s bed and create small depressions in it.
Middle course river features include wider, shallower valleys, meanders, and oxbow lakes. Lower course river features include wide flat-bottomed valleys, floodplains and deltas. As the river moves through the upper course, it cuts downwards. The gradient here is steep and the river channel is narrow. Vertical erosion in this highland part of the ...
River landforms can be divided into upper, middle and lower course features. These include steep V-shaped valleys, oxbow lakes and flood plains, respectively. Part of. Geography. Rivers and water.
Vertical erosion in this highland part of the river helps to create steep-sided V-shaped valleys, interlocking spurs, rapids, waterfalls and gorges. As the river erodes the landscape in the upper course, it winds and bends to avoid areas of hard rock. This creates interlocking spurs, which look a bit like the interlocking parts of a zip.
China's two major rivers, the Huang He (Yellow River) and the Chang Jiang (Yangzi or Yangtze River), as well as the Pearl River (Zhu Jiang) delta system marked by the Xi Jiang (West River) in southeastern China, have provided the framework for agricultural development and population growth throughout China's history.
The extent of China's territory was greatest under the last dynasty, called the Qing (Ch'ing) or Manchu dynasty between 1644-1912. China's territory was more extensive under the Qing empire than it is today. Bordering Nations. China is at the core of a cultural sphere or region known as East Asia.
However, while approximately 40% of the U.S. land can be cultivated, only 11% of China's land is arable. Much of the arable land in the United States, of course, is actually not used for farming but instead is used for pasture or has been developed for other uses.