rivers Flashcards
the hydrological cycle in a drainage basin:
precipitation
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interception ——> transpiration
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stem flow
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surface storage
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infiltration
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soil moisture ——> through flow
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percolation
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groundwater store
|
ground water flow
surface runoff ——> river carrying water to a lake or sea
|
evaporation
what does it mean when:
on a global scale, the hydrological cycle is a closed system
there are no inputs or outputs - nothing can enter the system or leave the system
what does it mean when:
on a local scales, within a drainage basin, the hydrological cycle is an open system
there are inputs (e.g. precipitation)
water table meaning
current upper level of saturate rock/soil where no more water can be absorbed
groundwater flow meaning
water flowing through the rock layer parallel to the surface
through flow meaning
water flowing through the soil layer parallel to the surface
surface runoff meaning
water flowing on top of the ground
evaporation meaning
water lost from ground/vegetation surface
transpiration meaning
water lost through pores in vegetation
ground water meaning
water stored in rock
percolation meaning
water seeping deeper through rock
soil moisture meaning
water help in the soil layer parallel
infiltration meaning
water sinking into the soil/rock form the ground surface
surface storage meaning
water held on the ground surface .e.g. puddles
interception meaning
water being prevented form reaching the surface/ground by vegetation or trees
precipitation meaning
any source of moisture reaching the ground .e.g rain, snow, frost
how might human activity impact the hydrological cycle in drainage basin
- deforestation would impact interception
-> less trees means water isn’t intercepted - deforestation would impact surface runoff
-> increases speed as less precipitation is intercepted
what is the source
the start of the river
what is the drainage basin
the area of land drained by a river and its tributaries
what is a confluence
where a tributary joins a larger river
what is the mouth
the end of a river (usually where the river meets the sea)
what is the water shed
the edge of the river basin
what is a tributary
a small stream that joins a larger river
how many ‘courses’ are there in a river
3 - upper, middle, lower
how does the long profile of a river change from source to mouth
the gradient decreases from source to mouth
upper - steep
middle - shallow
lower - fairly flat
what is the river valley like in the upper course
steep
what is the river valley like in the middle course
shallow
what is the river valley like in the lower course
flat
what is the river channel like in the upper course
narrow
what is the river valley like in the middle course
wider
what is the river channel like in the lower course
wide
what do we mean by ‘fluvial’
water
what do we mean by ‘processes’
things that a river does
examples of fluvial processes
erosion, transportation, deposition
erosion definition
wearing away of material
in the upper course of a river what process appears to be dominant
erosion
why does the river tend to erode vertically in the upper course
discharge is smaller and the river cuts down in a bid to get to sea level
rock is also resistant
why does a river tend to erode laterally in the middle course
material carried by the river can erode the banks
what tends to be the dominant process in the lower course of a river and why
deposition because the river slows down and uses energy
hydraulic action:
- occurs when the force of the river compresses air trapped in cracks in the banks
- the increased pressure weakens and gradually wears away the banks
abrasion:
- occurs when rocks carried by the river scrape and rub along the river bed and banks, wearing them down