Rivers Flashcards
Drainage Basin
An area of land drained by a river and its tributaries
Source
The start of a river
Tributary
A stream or river that flows into a larger river
Confluence
Where a tributary joins the river
Long profile shape
Upper course - Steep gradient
Middle course - Gentle gradient
Lower course - Very gentle gradient
Cross profile shape
Upper Course - Steep V-Shaped valley, narrow and shallow turbulent river
Middle Course - Valley with wider, flatter bed. Wider and deeper river
Lower Course - Very wide and flat valley. Wide, deep river with large sediment load
Why does the cross profile change over the course of the river?
- More water joins from more tributaries
- So more energy to erode larger channel
- Through processes such as abrasion, hydraulic action, etc
Why does velocity increase downstream?
- Upper course is shallower, so more energy is lost through friction between water and banks
- In the lower courses, water depth is greater so less water is in contact with the banks so river flows faster DESPITE SHALLOWR GRADIENT
Hydraulic Action
Where the force of water breaks rock particles away from the river channel
Abrasion
The eroding away of the river channel by rocks carried with the flow of the river
Attrition
- Stones carried by river hit each other
- Breaking down and rounding eachother
Solution / Corrosion
Mildly acidic river water dissolves limestone and chalk
Traction
Large boulders and rocks are rolled along river bed
Saltation
Small pebbles and stones bounce along river bed
Suspension
- Small particles are carried along by the water
- Such as silt or clay