3 Flashcards

1
Q

river carries it’s load:

A

solution
suspension
saltation
traction

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2
Q

solution

A

dissolved chemicals are carried along

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3
Q

suspension

A

tiny sediment particles carried along in current

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4
Q

saltation

A

small stones are picked up and dropped again

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5
Q

traction

A

large stones dragged along

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6
Q

river erosion

A

abrasion
hydraulic action
attrition
solution

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7
Q

abrasion

A

sand and pebbles dragged along wearing it away

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8
Q

hydraulic action

A

water into cracks, breaking it

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9
Q

attrition

A

wearing away as rocks knock together

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10
Q

solution

A

limestone dissolved by acidic rainwater

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11
Q

waterfalls formed:

A

1) bed of soft and hard rock
2) erosion of less resistant rock creating plunge pool
3) overhang collapses
4) waterfall takes new position leaving steep valley or gorge

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12
Q

weathering

A

biological
physical
chemical

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13
Q

biological weathering

A

small cracks allow roots to penetrate and force rocks apart

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14
Q

physical weathering

A

rock fills with rain, freezes, expands by 10% and breaks rock

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15
Q

chemical weathering

A

weak acids dissolve alkaline rocks

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16
Q

mass movement

A

process that cause rock material to move downslope

17
Q

rapid mass misvnt

A

-landslides and mudflow occur on railway cutting and along cliff coastline

18
Q

slow mass movement

A

(soil creep)

rain dislodging tiny soil particles each time it rains

19
Q

shape of valley affected by

A
  • rate of weathering
  • rate of mass movement
  • rate of removal of mass movement
20
Q

upper course

A

(buckden beck)

  • small stream/ tributary
  • steep gradient
  • small rapids and waterfalls
  • rainstorm increases river energy
21
Q

middle course

A

(river wharfe)

  • gradient = gentler
  • discharge = increase
  • velocity = increase
  • shape goes from V to U
  • flood plain widens
22
Q

lower course

A

estuary- river meets sea

river- wide and deep

23
Q

velocity

A

speed of river

hydroprop

24
Q

discharge

A

Volume of water flowing in River

area(width x depth) x velocity

25
Q

meanders change in valley

A

1) rivers bend in middle course and water flows naturally in a corkscrew pattern (helicoidal Flow)
2) -helicoidal flow sends river energy laterally
-Fastest current (thalweg) forced outer bend where it undercuts bank
3) Erosion creates narrow neck between two meanders
Oxbow lake created

26
Q

bradshaw model

A

summarises the changes to river characteristics from source to mouth

27
Q

increase

from upper to lower source

A
  • river discharge
  • channel width
  • channel depth
  • velocity
  • sediment load volume
28
Q

decrease

from upper to lower course

A
  • particle size
  • bed roughness
  • slope angle
29
Q

storm hydrograph

A

shows how river reacts to rainfall

30
Q

if lag time is shorter

A

heavy rain

impermeable surfaces

31
Q

if lag time is longer

A

less rainfall

rural (permeable surfaces)

32
Q

affect hydrograph shape

A
  • urbanisation

- deforestation

33
Q

antecedent rainfall

A

rainfall before

saturated soil

34
Q

surface run off

A

extra rain that soil can’t absorb

35
Q

quickness of surface run off

A
  • antecedent rainfall
  • permeable/impermeable
  • heaviness of rainfall
  • shape of river basin