Article abstract


Nature Geoscience 2, 653 - 658 (2009)
Published online: 16 August 2009 | doi:10.1038/ngeo610

Subject Categories: Geomorphology | Planetary science

Multiple origins of linear dunes on Earth and Titan

David M. Rubin1 & Patrick A. Hesp2


Dunes with relatively long and parallel crests are classified as linear dunes. On Earth, they form in at least two environmental settings: where winds of bimodal direction blow across loose sand, and also where single-direction winds blow over sediment that is locally stabilized, be it through vegetation, sediment cohesion or topographic shelter from the winds. Linear dunes have also been identified on Titan, where they are thought to form in loose sand. Here we present evidence that in the Qaidam Basin, China, linear dunes are found downwind of transverse dunes owing to higher cohesiveness in the downwind sediments, which contain larger amounts of salt and mud. We also present a compilation of other settings where sediment stabilization has been reported to produce linear dunes. We suggest that in this dune-forming process, loose sediment accumulates on the dunes and is stabilized; the stable dune then functions as a topographic shelter, which induces the deposition of sediments downwind. We conclude that a model in which Titan's dunes formed similarly in cohesive sediments cannot be ruled out by the existing data.

Top
  1. US Geological Survey, 400 Natural Bridges Dr., Santa Cruz, California 95060, USA
  2. Louisiana State University, Baton Rouge, Louisiana 70803, USA

Correspondence to: David M. Rubin1 e-mail: drubin@usgs.gov



MORE ARTICLES LIKE THIS

These links to content published by NPG are automatically generated.

NEWS AND VIEWS

Planetary science Titan's sticky dunes?

Nature Geoscience News and Views (01 Sep 2009)

The attraction of sand dunes

Nature News and Views (04 Jan 1996)


Extra navigation

Subscribe to Nature Geoscience

Subscribe

naturejobs

ADVERTISEMENT