River landscapes Flashcards
Physical weathering
Water gets into cracks in the rock.When the temperature falls below freezing, the water will expanded it turns into ice This expansion puts pressure on the rock around it fragments of rock break off
Biological weathering
Seeds that fall into cracks in the rocks will start to grow when moisture is present. The roots of the young plant force their way in and in time can break up rocks.
Chemical weathering
Rain water contains weak acids that can react with certain rock types. Carbonate in limestone are dissolved by weak acids and this causes the rock to break off or disintegrate.
Mass movement
When material moves down a slope due to the pull of gravity
Slumping
Happens on river banks, where part of it slips into the river. Common where the river passes clay as the dry weather makes clay contract and crack. Therefore rainwater gets into the cracks and the soil becomes saturated. Due to the pull of gravity, the large piece of weakened rock slips into the river. It is said to have slipped on the slip plane of saturated rock.
Abrasion
Material carried in the river is thrown against the river bed and banks by the force of the water,breaking of rocks.
Hydraulic action
The pressure of the water against the river bed.
Solution
Chemical reaction between certain types of rocks and minerals,wearing it away.
Attrition
Rocks in the water hit each other and break into smaller pieces.
Traction
Large rocks and boulders are rolled along the river bed.
Saltation
Small pebbles and stones are bounced along the river bed.
Suspension
Fine light material is carried along the river.
Solution [deposition]
Minerals are dissolved in the water and carried along in solution.
Deposition
The laying down of materials, such as sand and pebbles that are being transported by the river. Rivers deposit materials when they slow down and lose energy, such as on the shallow bank of a river
Change in the Characteristics of the River
Width/Depth:
The river will become wider/deeper as the amount of water in it
grows due to it being joined by tributaries as it moves towards the sea.
Change in the Characteristics of the River
Velocity:
As the river moves towards the sea and becomes deeper and wider, less water is in contact with the bed and banks, therefore, less friction occurs and the velocity increases
Change in the Characteristics of the River
Discharge
The amount of water in the river increases as the river moves towards
the sea because of the increase in volume due to it being joined by tributaries.
Change in the Characteristics of the River
Gradient:
The slope will become less steep as the river moves out of the hills and into flatter areas on its way to the sea
How does the UK’s seasonality affect river procceses?
In winter, the differences in temperatures between night and day can cause freeze thaw weathering on river banks, possibly causing the banks to collapse