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Barchan Dunes: These dunes are crescent-shaped with the tips pointing in the direction of the wind. Barchans are typically formed in areas with limited sand supply and a consistent wind direction. They move over time, and their size can change based on the strength of the wind. These dunes are common in deserts such as the Sahara and Central Asia, where the wind blows consistently in one direction.
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Longitudinal Dunes (Seifs): Longitudinal dunes, also known as seifs, are long, narrow ridges of sand that form parallel to the prevailing wind direction. These dunes occur in deserts with a more abundant sand supply and a variable wind direction, which causes the dunes to align in parallel lines. They are often larger and longer than Barchans and can be found in deserts like the Libyan Desert and Saudi Arabia.
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प्रश्न
Name two chief types of sand dunes.
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उत्तर
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Denudation
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अध्याय 10: Denudation - EXERCISES [पृष्ठ ९५]
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संबंधित प्रश्न
What do you mean by denudation?
How are meanders formed?
What are known as Deflation Hollows?
What is called denudation? Name the processes involved in it.
Give a technical term for the following:
The process in which a landform of lower level is upgraded to a higher level.
Describe the process of denudation and gradation.
Name the various processes involved in denudation.
What does the term denude mean?
In which region underground water is an effective agent of denudation.
What do you understand by the following term:
Gradation
