seif

sand dune
verifiedCite
While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions.
Select Citation Style
Share
Share to social media
URL
https://mainten.top/science/seif
Feedback
Corrections? Updates? Omissions? Let us know if you have suggestions to improve this article (requires login).
Thank you for your feedback

Our editors will review what you’ve submitted and determine whether to revise the article.

External Websites
Related Topics:
sand dune

seif, a long, narrow sand dune or chain of dunes, generally oriented in a direction parallel to the prevailing wind or in a direction resulting from two or more winds blowing at acute angles to each other. The dune crest consists of a series of peaks and gaps, and the steep, or slip, face may change sides of the dune according to changes in wind direction. Most seif dunes occur in the open desert and rest on a coarse sand sheet. Seifs, common in Libya and southern Iran, may range up to 90 m (300 feet) in height, with a width of six times their height and a length of up to 100 km (60 miles). They grow in height and width by the action of crosswinds and in length by the action of winds parallel to their axis.