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A mature river
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What is a river that erodes its channel wider rather than deeper?
mature.
What river erodes its channel wider rather than deeper?
A mature river erodes its channel wider rather than deeper. The gradient of a mature river is less steep than young rivers, and the water flows more smoothly. Examples of mature rivers are the Thames, Mississippi, and Ohio rivers.
What factors affect how a river erodes its channel?
The Factor is coastline
What is the deeper part of a river or harbor?
channel
What is the difference between vertical and lateral erosion?
Vertical erosion occurs when the river erodes it's bed, causing the deepening of the bed. Laterial erosion occurs when the river erodes it's banks, causing it's channel to widen.
What causes canyon formation?
Canyons such as the grand canyon usually a river cuts/erodes rocks and deposits the minerals some where else which through out years it grows deeper and deeper.
What is a frozen river that erodes slowly?
A frozen river that erodes slowly is called a glacier.
How is a river channel formed?
A river channel is formed by rock and soil of a stream being transported down, during this process the channels become wider and deeper.
What factors widen and deepen a river channel?
the river becomes excited and becomes wider deeper and more wet
Describe the cross profile of a river's lower course?
As a river continues its journey towards the sea, the valley cross section continues to become wider and flatter with an extensive floodplain either side of the channel. The river erodes laterally and deposition also becomes important. By the time it reaches the lower course the river is wider and deeper and may contain a large amount of suspended sediment.
What is the stage of rio grande river?
The Rio Grande is a Mature River because it is wider rather than deeper. It is not as steep, and the river has many tributaries.
What type of energy is involved when a river moves sediment and erodes banks?
Kinetic energy is involved when a river moves sediment or erodes its banks.
