Aeolian systems Flashcards

(54 cards)

1
Q

Define aeolian

A

Processes of erosion, entrainment, transportation, and deposition by the wind

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2
Q

Why is it harder to move particles on land than it water?

A

The difference in density is greater

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3
Q

How are grains on land held together?

A

Gravity, friction, vegetations, cements, moisture

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4
Q

What forces promote entrainment of grains on land?

A

Ballistic impacts and aerodynamic lift

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5
Q

What forces prevent entrainment of grains on land?

A

Weight, friction, drag, cohesive inter-particle forces

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6
Q

How are sand grains primarily transported? What does their transport and deposition allow?

A

As a bedload
Allows the construction of dunes

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7
Q

How are silt and clays primarily transported?

A

In suspension

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8
Q

What is a deflation lag deposit?

A

Formed by the grains that are too heavy to move e.g. gravel

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9
Q

Give the three ways (or combination of these ways) that sand can be carried as a bedload

A

Rolling/creep due to drag on the bed
Saltation
Reptation

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10
Q

Describe saltation in the bedload transport of sand grains

A

Particles are temporarily lifted into the airflow, collide with other particles, introducing a chain reaction of interparticle collisions
This process is the most important

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11
Q

Describe reptation in the bedload transport of sand grains

A

Saltating particles return to the bed and impacting other particles, causing them to hop short distances downwind

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12
Q

Where are aeolian processes most active and widespread?

A

Arid, hot/cold deserts
These cover ~30% of land surface

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13
Q

Why are grains in deserts so suseptible to aeolian processes?

A

They lack vegetation (to provide strength and cover) and moisture

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14
Q

Describe the back-erg of a dunefield

A

Represents the trailing, upwind margin of the erg

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15
Q

Describe the fore-wind of a dunefield

A

Represents the leading, downwind margin of the dunefield

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16
Q

Define an erg

A

Wind-formed desert landscapes characterised by extensive sand dunes that cover the terrain

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17
Q

Give three examples of geomorphic elements that can be associated with dunes

A

Zibars, sandsheets, interdunes

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18
Q

What are the six types of sand dune?

A

Barchan, transverse, linear, star, dome, parabolic

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19
Q

What is a stabilising aeolian system?

A

Develop where physical, chemical, or biogenic agents promote aeolian system construction and accumulation

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20
Q

What are the three classifications of aeolian systems?

A

Dry, wet, stabilising

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21
Q

Describe a dry aeolian system

A

Accumulation is controlled by aerodynamic configuration
Airflow deceleration causes sediment-laden winds to deposit some of their load

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22
Q

Describe a wet aeolian system

A

Accumulation is controlled by progressive water-table rise concomitant with ongoing aeolian activity

23
Q

Where do siliciclastic coastal dunefield typically occur?

A

Along humid, mid-latitude coasts

24
Q

Where do carbonate dunefields typically form?

A

Preferentially along mid-low latitude coasts, esp those bordering productive shallow marine platforms (supply of carbonate sediment)

25
How are aeolian processes inhibited in humid (inc. glacial regions) settings?
Vegetation and moisture
26
What is aeolian loess?
A layer of fine, wind-blown silt and clay particles
27
Where are loess deposits most typically found?
Areas that have experienced extensive glacial activity during past ice age Areas where strong winds carry fine grains from exposed surfaces (e.g. glacial outwash plains, river valleys, deserts)
28
What impacts do dust/sand storms have?
Reduced visibilty, productivty, resp diseases Fertisation of oceans (stimulates growth of phytoplankton)
29
What are the three scales of aeolian bedform?
Ripples, dunes, megadunes
30
What are the three types of small-scale ripple structures that occur on wind-blown surfaces?
Impact ripples, megaripples, adhesion ripples
31
What is the most widespread ripple type?
Wind ripples
32
Describe wind ripples
Low relief and form preferentially form the coarser-grained fraction of sand in transport
33
What are the three stages in the formation of wind ripples?
Initiation of development from perturbation on a bed Impact ripple spacing determined by saltation path length Upwind-facing stoss slope (subject to impact of infoming grains)
34
What generates a grain flow sand avalanche?
Gravitational collapse of dry, loose sand on aeolian dune/megadune lee slopes inclined at the angle of repose (~32-36deg)
35
What is an aeolian grain flow strata?
Thick package of multiple stacked aeolian grain flow avalanche deposits
36
When does gravity-driven grain fall occur?
Where wind carrying clouds of saltating grains over a dune brink decelerates as it passes into the lee-side depression, resulting in a reduction in sediment carrying capacity
37
Give another example of when gravity-driven grain fall can occur
On the apron of a dune where secondary cross-wind airflow is insufficient to form ripples
38
Describe what happens when net aeolian sediment budget is positive
Accumulation occurs where bedforms may climb over one another at varying angles Sets and cosets of cross strata are produced
39
Describe the sets of cross strata formed when bedforms climb over one another
Contain smaller-scale facies units of wind-ripple, grainflow, grainfall, and plane-bedded strata Therefore, dune elements are larger scale strata units
40
Why is one bedform truncated by another?
They climb at low angles, the lower bedform is accumulated as the second overrides it
41
Define aeolian interdunes
Elongated, relatively flat and sandy landforms that exist between larger sand dunes in desert and arid environments
42
Describe a dry interdune
Water table is not in contact with depositional surface
43
Describe a damp interdune
Capillary fringes of the water table are in contact with the depositional surface
44
Describe a wet interdune
Water table is in contact with the depositional surface
45
How do adhesion strata arise?
Arise from the adhesion of moving grains to a damp surface e.g. a damp interdune
46
Describe adhesion strata
Low relief Sub-horizontal structures with irregular surfaces
47
Describe megadunes (draas)
Support development of superimposed dune-scale bedforms
48
Describe a compound draas
Where a smaller dune is superimposed on a larger dune of the same morphological type
49
Describe a complex draas
Where a smaller dune is superimposed on a larger dune of a different morphological type
50
What is an aeolian sand sheet?
Areas of sand accumulation characterised by flat areas of impact wind ripples Limited by sediment supply
51
What is a zibar?
Low relief ridges and domes with gently inclined sloping surfaces
52
What is required for the long-term preservation of aeolian sequences?
The strata is placed below a regional baseline, below which erosion does not occur
53
What does subsidence allow?
It is the principal agent that generates accommodation and promotes preservation
54
Give two examples of how aeolian strata can achieve long-term preservation
Accumulation occurs in a subsiding basin Accumulation occurs below the water table and is protected from deflation