rivers 🏞️ Flashcards

(40 cards)

1
Q

mouth

A

the point at where the river reaches the sea/lake

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2
Q

confluence

A

the point at which a tributary flows into another river

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3
Q

watershed

A

a ridge of high land that forms the boundary between 2 adjacent drainage basins

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4
Q

drainage basin

A

the area drained by a river and its tributes

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5
Q

source

A

the start of a river, it can be a hollow where water accumulates or a natural spring where water reaches the surface

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6
Q

tributary

A

a small stream that flows into a larger one

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7
Q

river

A

a large natural stream of flowing water that empties into another water body ( lake , sea other river )

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8
Q

the drainage basin system

A

precipitation
interception
evaporation
surface storage
infiltration
surface run off -( evaporation )
soil moisture storage -( through flow , channel flow )
percolation
ground water storage -( ground water flow )

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9
Q

transpiration

A

water stored on the plants / leaves turn into vapour and spreads into the atmosphere

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10
Q

why does the amount of interception vary from place to place

A

some areas have more vegetation than others

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11
Q

why does the amount of interception vary at different times of the year

A

trees shed their leaves in the winter if it rains / snows the water is able to get into the ground

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12
Q

river processes

A

erode, transport , deposition

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13
Q

erode

A

hydraulic action
attrition
corrosion
abrasion

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14
Q

transport

A

saltation
solution
traction
suspension

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15
Q

river long profile

A

shows a change in the height of the course of a river from its source to its mouth. al long profile is usually concave and the slope becomes more gentle towards the mouth of the river

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16
Q

upper profile

A

profile is steep
reduces hight very quickly
a lot of potential energy because of the steep drop
dominated by vertical erosion
narrow and steep sided
has little water volume

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17
Q

middle profile

A

the gradient of the profile has reduced
lateral erosion is more as more of the profile has reduced
lateral erosion is more important
the channel is wider and the valley sides are less steep

18
Q

lower profile

A

less erosion , more deposition
potential energy has been replaces by energy from a high water volume
the river carries a large amount of load

19
Q

waterfall

A

the softer rock retreats backwards upstream
the overlying then becomes unsupported and falls / brakes away
the fallen material gets swirled around in the plunge pool

20
Q

meanders

A

a bend in a river
as the river gets more load it becomes more difficult to move along a straight channel
where the water hits the bank it erodes material in the areas where the water is travelling slower, the water has less energy and so deposits the eroded material

21
Q

how are meanders formed

A

As the water flows around the bend it is pushed further out causing the water flowing on the outside of the bend to be faster.
This means that erosion takes place and the bank is undercut by the process of hydraulic action and abrasion. This forms a river cliff.
On the inside the flow is slower and therefore deposition occurs to form a slip off slope or point bar.

22
Q

Potholes

A

If the river bends is uneven, pebbles become trapped in holes
Swirling currents cause the pebbles to rotate and erode circular holes in the river bed
This is done through the process of corrosion whereby sediment is trapped in the pot hole
Score away the base and the sides of it making it deeper and wider

23
Q

Oxbow Lake

A

Before
Lateral erosion
Land being eroded on both sides
Deposition
Line of fast flow

After
Neck of land removed by erosion of the banks from two side sides often at the time of flood
Position use of the ends of the cut off lake
Stagnant water
Meander Island
Oxbow Lake
Rivercliff

24
Q

Flood plain

A

A floodplain is an area of flat land either side of the river, which is often marsh. When a river floods it carries the load from the river onto the land either side. The big material is deposited first next to the river as it heavier. This builds up the banks making them taller these are called levees. The fine muddy material called alluvium is carried further. As the water seeps into the ground or flows back into the river, the sediment is left behind leaving the land much more fertile during normal flow the river deposits material from its load on the river bed causing the river to be lower than the surrounding floodplain.

25
Deltas
As the speed of flow slows down, the energy is reduced and therefore the river cannot carry it load, especially if the river is heavily laden with soil and there is an absence of major title flows or currents. When sediment especially clay comes into contact with the saltwater its clumps together and becomes heavier., as a result of the river deposit sediment. As the settlement build up growth of vegetation raises as above sea level and distributor start to form where the river splits into many channels around the deposited sediment. This process is repeated and therefore further accumulation occurs over time.
26
River flooding
The water in the river is called the river discharge A flood is an overflow of a large amount of water beyond this normal limits, especially over what is normally dry land The more the water gets intercepted the less run-off and discharge there is
27
Factors affecting river discharge
When plants absorb or intercepts rainfall, it decreases discharge Impermeable rock increases discharge Steep pill increase discharge flatlands decrease discharge Totally packed, so you won't have the ability to absorb rainfall thus increasing run-off Saturated soil would already be full of water which would increase discharge Channel rainfall away for treatment increases discharge Surfaces were infiltration as possible decreases discharge
28
Bangladesh case study
Physical Three rivers meet in Bangladesh 70% of the country is less than one meter above sea level tropical cyclones from the Bay of Bengal bring heavy rain and storm waves. Snow melts in the Himalayas in summer bringing more water 10% of the land is covered in rivers, lakes and swamps south Asia has a monsoon climate and experiences a wet season between May and September bringing 2000 mm of rain increased sedimentation in the river channels from eroded soil causes river bends to rise reducing your capacity. Global warming is causing sea levels to rise.
29
Bangladesh case study
Economic GDP per capita is about $380 so there's little money to spend on the river management
30
Bangladesh case study
Social Population growth in cities like a Dhaka is increasing the size of urban areas population growth in Nepal and North India has led to rapid deforestation
31
Hard engineering
Involves putting in place of physical barrier between the land and the river
32
Soft engineering
Involves working with nature to protect places from flooding
33
Increase capacity
Get a bigger river to hold more water depending the dam
34
Increase velocity
Get the water through the river, faster cementing the dams
35
Reducing discharge
Slow down the flow of water into the river
36
River investigation
Precaution Consider velocity Nature of the rocks Do not drink the water Work in pairs
37
Depth
The measurement of death should be completed at a regular intervals across the whole with. This ensures a full picture of the changes in depth across the whole channel it also allows a mean depth to be calculated to use in the calculation of river discharge. To take accurate depth measurements: Work out the distance Place a meter rule into the water Ensure the meter rulers placed sideways on with the flat side facing the bank With the distance from the bed to the surface of the water Repeat this across the river
38
Width
The measurement of the width is taken where the water surface comes into contact with the river banks Take accurate measurement: Measure from the point with a dry bank meats the water on one side to the point where the dry bank meets the water on the opposite side Ensure the tape is held taught and does not touch the water
39
Wetted perimeter
The part of a river that touches the water
40