Page 323 - Fundamentals of Geomorphology
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306 PROCESS AND FORM


              Table 12.3 A classification of dunes
              Primary dune forms Criteria for subdivision Secondary dune forms  Description

              Free          Morphology or orientation:
                            Transverse       Transverse       Asymmetric ridge
                                             Barchan          Crescentic form
                                             Dome             Circular or elliptical mound
                                             Reversing        Asymmetric ridge with slip faces on either side of
                                                                the crest
                            Linear           Seif             Sharp-crested ridge
                                             Sand ridge       Rounded, symmetric ridge, straight or sinuous
                            Star             Star             Central peak with three or more arms
                                             Network          Confused collection of individual dunes whose
                                                                slip faces have no preferred orientation
                            (Sheets)         Zibar            Coarse-grained bedform of low relief and
                                                                possessing no slip face
                                             Streaks or stringers or  Large bodies of sand with no discernible dune
                                              sand sheets       forms

              Anchored      Vegetation and topography:
                            Topography       Echo             Elongated ridge lying roughly parallel to, and
                                                                separated from, the windward side of a
                                                                topographic obstacle
                                             Climbing dune or  Irregular accumulation going up the windward
                                              sand ramp         side of a topographic obstacle
                                             Cliff-top        Dune sitting atop a scarp
                                             Falling          Irregular accumulation going down the leeward
                                                                side of a large topographic obstacle
                                             Lee              Elongated downwind from a topographic obstacle
                                             Fore             Roughly arcuate with arms extending downwind
                                                                around either side of a topographic obstacle
                                             Lunette          Crescent-shaped opening upwind
                            Vegetation       Vegetated sand   Roughly elliptical to irregular in plan, streamlined
                                              mounds            downwind
                                             Parabolic        U-shaped or V-shaped in plan with arms opening
                                                                upwind
                                             Coastal          Dunes formed behind a beach
                                             Blowout          Circular rim around a depression
              Source: Based on Livingstone and Warren (1996, 74–101)




              upon the slope of the obstacle. When the upwind slope  zone of slightly lower wind velocity just beyond the crest
              of an obstacle is less than around 30 , sand blows over it.  of an obstacle. Falling dunes form in the lee of an obsta-
                                       ◦
              When it is above 30 , then sand is trapped and a climb-  cle, where the air is calmer. If the obstacle is narrow, then
                            ◦
              ing dune or sand ramp forms. If it exceeds 50 , then an  sand moving around the edges may form lee dunes that
                                              ◦
              echo dune forms at an upwind distance of some thrice the  extend downwind. Lunettes are crescent-shaped dunes
              height of the obstacle. Cliff-top dunes may form in the  that open upwind and are associated with pans (p. 299).
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