Paper 1: River processes Flashcards

1
Q

tributery

A

small river that flows into a main river

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2
Q

vertical erosion

A

-downwards erosion of the river bed

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3
Q

drainage basin

A

land drained by a river and its tributaries

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4
Q

river channel

A

slot of land that a river flow in

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5
Q

confluence

A

place where 2 rivers meet

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6
Q

load

A

material carried by river

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7
Q

lateral erosion

A

sideways erosion of river

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8
Q

watershed

A

high land around edge of river basin

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9
Q

source

A

start of river

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10
Q

mouth

A

end of river

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11
Q

long profile

A

journey river makes to sea

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12
Q

upper course long profile

A

-high
-steep
concave shaped

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13
Q

middle course long profile

A

-flatter relief
-gentle lope

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14
Q

lower course long profile

A

-below/very close to sea level
-flat

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15
Q

erosion

A

-wearing away of river bed/banks
-breaking rocks carried by river

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16
Q

transport

A

-movement of material along river course

17
Q

deposition

A

-dropping of river load when river lacks energy to transport it

18
Q

cross profile

A

-taken sideways across river channel/valley

19
Q

channel cross-profile

A

-includes river only

20
Q

valley cross profile

A

-includes channel
-valley floor
-slopes at the sides of valley

21
Q

velocity

A

speed of river flow

22
Q

discharge

A

-volume of water passing through a given point on a river
-cumecs

23
Q

river channel cross section - upper

A

narrow channel
-shallow
-little discharge

24
Q

river channel cross section - lower

A

-becomes deeper
-wider
-more discharge

25
what happens to velocity downstream
-increases -as discharge increases
26
velocity upstream
-low -little water in river crashes against rocks -lots of friction slows speed
27
bedload size of upper course
-large boulders
28
valley of upper course
-steep -v-shaped
29
valley of lower course
-u -shaped -wider
30
scree
deposited material from valley in channel
31
v shaped valley
-wide at the top -narrower towards base -
32
interlocking spurs
-ridges of hard rock that project on alternate sides of river valley where river flows -only in upper course
33
why do interlocking spurs only exist in the upper course
-rock is hard -slow to erode as less energy of river
34
erosion in upper course
-vertical erosion -little energy so it is focused here
35
why do v shaped valleys occur
-freeze-thaw weathering occurs on upper sides of valley -widens top of valley but base is narrow
36
freeze-thaw weathering
-water gets into cracks of rock -freeze at night = expands crack -melt during the day -shatter rock