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A large dune complex is called a dune field, [7] while broad, flat regions covered with wind-swept sand or dunes, with little or no vegetation, are called ergs or sand seas. [ 8 ] [ 9 ] [ 10 ] Dunes occur in different shapes and sizes, but most kinds of dunes are longer on the stoss (upflow) side, where the sand is pushed up the dune, and have ...
Issaouane Erg, Algeria Linear Dunes, Namib Sand Sea. An erg (also sand sea or dune sea, or sand sheet if it lacks dunes) is a broad, flat area of desert covered with wind-swept sand with little or no vegetative cover. [1] The word is derived from the Arabic word ʿirq (عرق), meaning "dune field". [2]
Dune system – Hill of loose sand built by aeolian processes or the flow of water; Estuary – Partially enclosed coastal body of brackish water; Firth – Scottish word used for various coastal inlets and straits; Fjard – Glacially formed, broad, shallow inlet; Fjord – Long, narrow inlet with steep sides or cliffs, created by glacial activity
A nabkha, nebkha or nebka is a type of sand dune. Other terms used include coppice dune and dune hummock or hummocky dune, but these more accurately refer to similar, but different, sand dune types. [1] Authors have also used the terms phytogenic hillock, [2] bush-mound, shrub-coppice dune, knob dune, dune tumulus, rebdou, nebbe, and takouit. [3]
A sandy depression formed when wind erodes into patches of bare sand on otherwise vegetation-stabilized sand dunes at the margins of coastal and arid ecosystems. bluff A steep slope or cliff marking the outer margin of a floodplain, especially one formed as the river erodes the concave bend of a meander. See also cut bank. bocage
Sand dune is a color that resembles the color of a sand dune composed of dark colored sand. The first recorded use of sand dune as a color name in English was in 1925. [17] The normalized color coordinates for sand dune are identical to the color names drab, mode beige and bistre brown, which were first recorded as color names in English ...
The dunes emulate soliton behavior, but unlike solitons, which flow through a medium leaving it undisturbed (similar to waves passing through water), the sand particles themselves are moved. When the smaller dune catches up the larger dune, the winds begin to deposit sand on the rear dune while blowing sand off the front dune without ...
Foredunes may begin as shadow dunes that form in the wind shadows of clumps of vegetation. [2] Several shadow dunes may eventually join to form an incipient foredune. [3] When an incipient foredune reaches a height of about 1.5 feet (0.5 m), it has a significant wind shadow of its own.