Fluvial Forms Flashcards

(72 cards)

1
Q

List 5 fluvial bedforms

A
Ripples
Dunes
Plane bed
Antidunes
Obstacle marks
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2
Q

What are fluvial bedforms similar to?

A

Aeolian bedforms

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3
Q

What is the medium for fluvial bedforms?

A

Water

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4
Q

What is the medium for aeolian bedforms?

A

Air

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5
Q

What does larger material require to be moved?

A

Higher stream power

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6
Q

What does the presence of fluvial bedforms depend on?

A

Grain size

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7
Q

What are horizontal bedplanes indicative of?

A

Lower stage plane beds

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8
Q

In which direction do ripples migrate overtime?

A

Down flow

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9
Q

Which side do ripples erode?

A

Upstream side

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10
Q

Which side do ripples deposit?

A

Downstream side

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11
Q

Give a place where ripples can be seen?

A

The beach

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12
Q

What is meant by transient?

A

Adjust quickly to change

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13
Q

Are ripples transient?

A

Yes

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14
Q

What energy conditions are required for ripples to form?

A

Lower energy conditions

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15
Q

What transportation process allows ripples to form?

A

Suspension

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16
Q

What do ripples have a high rate of?

A

Aggradation

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17
Q

Are dunes visible?

A

Yes, they poke out of the water to a greater extent

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18
Q

What do dunes cause?

A

Surface waves that are out of phase with the water bed.

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19
Q

Is the amplitude of dunes higher or lower than that of ripples?

A

Higher

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20
Q

What can the amplitude of dunes reach?

A

10s of cm to 10s of m

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21
Q

What shows migration in dunes?

A

Cross stratification

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22
Q

In which direction do dunes migrate?

A

Downflow

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23
Q

How do dunes migrate?

A

By accretion of the lee side

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24
Q

Why are dunes in dynamic equilibrium?

A

The stoss side is eroding and the lee side is depositing

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25
What are two important features of the upper stage plane bed?
Coarser material than lower stage | Some rocks
26
In what plane bed would you find ripples?
Lower stage plane bed
27
In what plane bed would you find dunes?
Lower stage plane bed
28
What are antidunes?
The opposite of dunes
29
What type of feature are antidunes?
Erosional
30
In which direction do antidunes migrate?
Upflow
31
What waves are antidunes associated with?
Breaking waves
32
What is the water flow like around antidunes?
Shallow but fast
33
In which way do antidune beds dip?
Upflow
34
Why is the stoss side of antidunes preserved?
Due to the dip
35
Which side of the antidune is eroded?
Lee side
36
Which side of the antidune moves upward?
Crest side
37
How long are antidunes preserved for?
They are very rarely preserved
38
What are two features of cluster bedforms?
Rocks dip into the flow | Coarser material
39
List 4 obstacle marks
Ice blocks Secondary bedforms Vegetation Anthropogenic sources
40
What flow can ice blocks create?
Horse shoe flow
41
What can ice blocks cause?
Scouring due to horse show flow
42
What changes overtime in rivers?
Discharge
43
What two things do bars require?
Cohesionless sediment | Bedload
44
Why are bars difficult to define?
They depend upon flow depth and discharge
45
What are bars?
Attachments to channel margins
46
Where can bars be found?
Mid channel
47
What are bar types often associated with?
Channel morphological type
48
What transportation process causes bars?
Suspended load
49
Are bars formed in low or high energy environments?
Low energy
50
What bars can braided rivers have?
1st, 2nd and 3rd order bars
51
In what environments do braided rivers occur?
In a number of enviroments
52
Where are braided rivers usually found?
Where there is a lot of sediment
53
Give two examples of wondering gravel bed rivers
River Coquet, Northumberland | Fraser River, British Columbia
54
What can be done to find the age of island bars?
Tree coring
55
What can affect the location of erosion/ deposition?
Positioning of flow cells
56
What happens as the river channel widens? (3)
Flow reduces Sediment transport reduces Change in the type of material transported
57
What are the main features of Anastomosing rivers?
Parallel channels | Aligned by natural levees with flood basins inbetween
58
Define Anastomsing river
"A type of river channel with multiple interconnected, coexisting channel belts on alluvial flood plains, which most often form under low energy conditions near a local base level" Makaske 2001
59
When do braided rivers occur?
When erodibility of bank particles is more than their transportability
60
When do meandering rivers occur?
When erodibility and transportability of bank particles are equal
61
When do straight rivers occur?
When transportability of bank particles is higher than erodibility
62
What is the spacing like for pools and riffles?
It is regular
63
What property changes in pools and riffles can occur and why?
Major changes in hydraulic properties depending upon flow stage
64
What hypothesis is associated with pools and riffles?
Velocity reversal hypothesis
65
What is the velocity reversal hypothesis?
Velocities in pools increase at a higher rate than in riffles
66
Can rivers be damned by their own levees?
Yes
67
When do river terraces form?
After glaciers melt
68
Why do river terraces form after glaciers melt?
There is less discharge
69
What do river terraces reflect a change in?
River channel change in water and sediment flux
70
Briefly explain the magnitude and frequency concept
Argument over whether frequency of floods is more important than intensity. Medium magnitude floods occurring over intermediate timescales achieve most work in terms of sediment transport.
71
What is avulsion?
Rapid channel change
72
What is river terrace formation an example of?
Complex response