Sand Dunes Flashcards

0
Q

Formation: Dunes have a downwards ‘lee’ slope and

A

An upwards ‘stoss’ slope.

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1
Q

Formation: An obstacle, such as a

A

Rock, allows transported particles to settle around it. The particles build up to form a dune.

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2
Q

Formation: The wind moves particles up the

A

Stoss slope by saltation. The particles accumulate on the lee slope.

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3
Q

Formation: As material becomes unstable,

A

It moves down the lee slope, resulting in dune migration downwind.

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4
Q

Scale: Greater dune height =

A

Slower movement.

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5
Q

Scale: Taller dune =

A

Greater volume.

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6
Q

Scale: Ripples - usually measured in

A

cm to 10’s of cm.

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7
Q

Scale: Ripples - Wind blows on

A

Sand crest, ripple crests are perpendicular to wind direction.

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8
Q

Scale: Ripples - Wavelength of ripples is

A

Determined by the average distance sand particles jump during saltation.

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9
Q

Scale: Dunes - Wavelengths measured in

A

10’s - 100’s metres.

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10
Q

Scale: Dunes - Height measured in

A

Metres.

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11
Q

Scale: Dunes -

A

Accumulation of sand, blown into a mound by the wind.

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12
Q

Scale: Draas - Large dunes, measured in

A

Kilometres.

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13
Q

Scale: Draas - Height measured in

A

Metres.

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14
Q

Form: Crescentric dunes - (3)

A

Crescent shaped.
Segment is wider than it is long.
In areas with a single wind direction.

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15
Q

Form: Crescentric dunes - Barchan dunes -

A

Crescents with horns pointing downwind.

16
Q

Form: Crescentric dunes - Transverse - (3)

A

Asymmetric ridges, transverse to wind direction.
1-30 m high.
Move faster than any other dune type.

17
Q

Form: The shape &

A

Relative position of slip faces.

18
Q

Form: Linear dunes (Seif dunes) - (4)

A

Slip faces occur on both sides.
Can be 100m high and 100km long.
In areas with two wind directions.
Long, straight sand ridges.

19
Q

Form: Star dunes - (4)

A

Can be over 100m high.
Wind blows from all directions.
Base resembles a star.
Isolated hills.

20
Q

Form: Parabolic dunes - (4)

A

Wind of single direction.
Some vegetation.
Open end of U points upwind.
U-shaped.

21
Q

Form: Reversing dunes - (2)

A

Asymmetric ridge.

Winds are balanced from opposite directions.

22
Q

Complexity: Simple dunes - (3)

A

Basic forms.
Minimal number of slip faces.
Wind regime and intensity hasn’t changed since formation.

23
Q

Complexity: Compound dunes - (2)

A

Large dunes with smaller dunes superimposed.

Wind hasn’t changed direction, but has decreased in intensity.

24
Q

Complexity: Complex dunes - (2)

A

Large dunes with smaller dunes of different type superimposed.
Significant change in wind direction and intensity.