Asymmetrical ridge (in contrast to longitudinal straight dunes, which are symmetrical) with steep leeward slope and gentle windward slope (Fig.
1). Transverse ridges have one slipface. They show largely horizontal strata (apparent dip) in cross sections parallel to crest, in contrast to curving strata of barchanoid ridges viewed in similar sections (McKee
1979, p. 406).
Wind Direction Geographical Information Classic Form Prevailing Wind Sediment Supply
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