River processes, long profiles and cross profiles

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GCSE GCSEs (Geography) Flashcards on River processes, long profiles and cross profiles, created by a a on 28/04/2014.
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Created by a a over 11 years ago
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Question Answer
What is abrasion? Pieces of material are carried in the water and wear away the bank like sandpaper
What is attrition? Material carried along the river collides into other pieces of material and breaks into smaller pieces
What is hydraulic action? The force of water hitting the river bank/ bed which then breaks pieces off
What is solution erosion? Some rocks (like limestone) are dissolved by acids in the water, which then go on to corrode the river bank/ bed
Name 4 types of erosion. Abrasion, attrition, hydraulic action and solution erosion
Name 4 types of transportation. Traction, saltation, solution and suspension
Define erosion. The removal of material
Define transportation. The movement of the load along the river channel
Define traction. Large boulders and rocks are rolled along the river bed by the rising power
Define saltation. Sand sized particles are bounced along the river bed
Define suspension. Small particles are carried along by the river
Define solution (transportation). Material is dissolved into the river and then transported
Define deposition. Material is dumped at a point along the river after being carried from further upstream
What is the difference between lateral and vertical erosion? Lateral erosion- wearing away the river banks, widening the channel Vertical erosion- wearing away the river bed, making the channel deeper
Describe the cross profile and river channel in the upper course of a river. Cross profile- steep 'v' shaped valley. Tall narrow cross profile. River channel- Narrow channel, shallow water
Describe the cross profile and river channel in the middle course of the river. Cross profile- profile widens, less deep and the valley sides are less steep. River channel- becomes wider and deeper
Describe the cross profile and river channel in the lower course of a river. Cross profile- the valley is very broad. The sides are a long way from the river. The valley is gently sloping and low lying River channel- deepest and widest part of the river
How does the gradient of a river change as you move from the source to the mouth? The gradient becomes much less steep
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