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12 Cards in this Set
- Front
- Back
Cards by adac - please rate and favorite.
Sourced mainly from Thomas D. S. G., 2011, Arid Zone Geomorphology: Process, Form and Change in Drylands - Chapter 19 (written by Nick Lancaster). I recommend studying my cards in order, at least for the first few tries. |
My cards are designed so you describe the subject, rather than naming something after seeing the description. My method will better prepare you for short answer and essay questions.
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Name as many types of dunes as you can think of.
(We will focus mainly on two types) |
Two types we will focus on:
- Crescentic - Linear Others: - Star - Parabolic - Zibars and sand sheets (Refer to text books for more information on these) |
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Dune type: Crescentic dunes
- Wind regime (direction) - Describe their morphology |
- Unidirectional wind regime
- Crests aligned normal to the direction of sand transport. Typically elliptical in shape with a concave lee face and horns extending downwind. |
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Isolated crescentic dunes form under what conditions? What is another name for these dunes?
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Isolated crescentic dunes form in undersaturated sand transport conditions (sand supply low relative to wind capacity to transport sand).
Also known as barchans. |
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How do crescentic mega dunes form?
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Mega dunes form from the super-imposition of smaller crescentic dunes on their stoss slopes (windward slopes).
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Name the broad varieties of linear dunes.
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Simple, compound and complex.
The latter two occur as mega dunes. |
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Identify two simple linear dune types.
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- Sinuous; relatively short dunes (aka seif dunes)
- Longer, straight, vegetated dunes (common in Australia) |
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Describe compound linear dunes.
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Consist of several narrow, closely spaced, seif-like ridges on the crest of broad linear plinths which are spaced as much as 2.5km apart.
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Describe complex linear dunes
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Comprised of relatively straight, continuous, linear ridges on which other dunes super impose.
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What wind regime do linear dunes form in?
(Currently a debatable issue) |
Generally accepted to be bidirectional wind regimes with the two modes separated by 90 degrees or more.
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How do linear dunes extend in relation to wind?
Eg. Perpendicular? Parallel? Downwind? Upwind? |
Tend to extend downwind but may also migrate laterally since sand transport by bimodal winds is rarely equal.
Some linear dunes form parallel to the dominant wind direction - this occurs mainly where vegetation partially stabilizes the sand or topographic obstacles anchor the sand in place. |
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Controls of dune morphology.
Name the main determinant of dune morphology. What are some subordinate controls? |
Dominant control: Directional variability of wind regime.
Subordinate controls: Wind speed, grain size and vegetation. |