Fluvial Processes and Landforms Flashcards

1
Q

Fluvial Process

A

processes that involve running water

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2
Q

Valley

A

area where drainage system clearly established

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3
Q

interfluve

A

higher land above valley walls that separates adjacent valleys

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4
Q

watershed

A

AKA drainage basin, consists of valley bottom, sides, portions of surrounding interfluves

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5
Q

Stream order

A

1st - smallest
gets bigger w. numbers

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6
Q

Erosion by overland flow

A

1) rain drops fall –> splash erosion, causing particles to move downhill
2) sheet erosion = water flows down surface as thin sheet, transporting particles
3) Moves onto rill, which converge into gullies

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7
Q

How does sediment get into river

A

1) weathering of rock (breaks into smaller particles)
2) mass wasting (sediment moves down)
3) erosion - 3 steps (stream erosion, transportation, deposition)

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8
Q

What determines erosive capacity of stream

A

1) direct hydraulic power of moving water
2) rocks, boulders, silt the stream carries contributes to erosion
3) chemical action = hydrolysis + corrosion
4) flow speed

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9
Q

what affects flow speed

A

1) gradient (steeper gradient, faster flow)
2) shape of channel (more narrow, goes faster)
3) volume (more water, higher flow)

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10
Q

1) High competence + capacity leads to
2) low competence + capacity leads to

A

1) erosion
2) deposition

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11
Q

Stream load

A

1) material brought by water
2) 3 components:
1) dissolved load, includes minerals
2) suspended load = fine clay/silt particles that literally are suspended in water
3) bedload = larger rock fragments

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12
Q

Saltation vs traction (relates to bedload)

A

1) saltation = think of hops of smaller rock
2) traction = larger rocks which slide/roll down streambed

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13
Q

Stream Competence

A

1) stream competence = measure of particle size stream can transport, mainly depends on flow speed (double speed, 4X particle size)
2) measure of particle diameter
3) influenced by velocity

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14
Q

stream capacity

A

1) measure of amount of solid material stream can transport, expressed as volume
2) fluctuates over time
3) influenced by velocity + amount of water

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15
Q

Flood recurrence interval

A

1) probability of given-size flood
ex: 100 year flood = 1 in 100 chance of happening more than once a year

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16
Q

Stream channel patterns

A

1) straight
2) sinuous
3) meandering
4) braided

17
Q

Straight stream channel pattern

A

1) short + uncommon (generally manmade)
2) strong control by underlying geological structure
3) thalweg - line created by deepest water - meanders even in straight channel

18
Q

Sinuous channels

A

1) Winding + occur in every type of topographic setting
2) very common
3) common in high latitude

19
Q

Meandering channel

A

1) follows serpentine course, forming VERY SMOOTH curves
2) occurs in FLAT GROUND with suspended load

20
Q

Braided Channels

A

1) multiple interwoven + interconnected channels
2) takes place in heavy sediment load (Gravel) + in areas with prominent dry seasons
3) active channels of braided stream make cover less than 1/10 width of full channel

21
Q

Downcutting (valley DEEPENING)

A

1) lowering of streambed via hydraulic power
2) occurs when stream is very fast or has high volume
3) produces V-shaped cross section

22
Q

Base level

A

1) limit to amount of downcutting a stream can do
2) at a gradient –> allows stream to flow

23
Q

Sea Level

A

Absolute, ultimate base level for streams

24
Q

graded stream

A

when stream reaches dynamic equilibrium
most streams do not achieve this throughout course all the time

25
Q

Knickpoint migration

A

1) irregularities in channel + common result of abrupt changes in bedrock resistance
2) rapid when bedrock consists
3) Basically like a retreating cliff that is breaking apart because of water

26
Q

Lateral erosion (widening valley)

A

1) Happens in meandering rivers
2) Erosion on outside of banks
3) deposition in inside

27
Q

How can stream lengthen its valley

A

1) headward erosion
2) delta formation

28
Q

Delta formation
(lengthening)

A

1) lengthening at seaward end
2) process that occurs when a river carrying sediment slows down and empties into a larger body of water, forming new land + lengthening river (forming distributaries)

29
Q

What is headward erosion?

A

1) when stream erodes soil/rock at head of stream –> lengthening it

30
Q

Floodplains

A

1) low-lying nearly flat valley floor that is periodically inundated with floodwaters
2) outer points of meanders

31
Q

bluff

A

1) steep bank or cliff that forms along a river valley due to erosion and land movements
2) edge of lateral erosion

32
Q

Cutoff meander/oxbow lake (cutoff meander –> oxbow –> meander scar)

A

1) cutoff meander = when an new channel is created, cutting water off from old loop
2) oxbow lake = when cutoff portion filled with water for temporary period of time (not connect to river anymore) –> eventually dry up becoming meander scars

33
Q

Natural levees

A

1) raised areas of sand and mud that form along the banks of rivers and streams
2) because when flooding –> reduced competence + capacity –> therefore drops heavier sediment

34
Q

Yazoo streams

A

1) tributary stream that flows parallel to a larger river within its floodplain for a considerable distance before joining it
2) water that cannot go back –> bc of natural levees

35
Q

Flood controls for rivers

A

1) dams = flood control + to ensure enough water for ships to go through
2) artificial levees = works BUT if it fails –> often catastrophic

36
Q

Cutbank

A

High velocity –> results in increased competence/capacity on the outside of the meanders – > increased erosion

37
Q

PointBar

A

decrease velocity on inside –> reduced competence/capacity on inside of meanders –> increased deposition