Most bed sediments in estuaries and tidal basins are a mixture of sand and mud, with spatial gradients in the sand/ mud content, typically with sandy outer areas near the inlet and fining in the landward direction. These gradients may be gradual or abrupt, and cover large spatial scales (e.g., a tidal basin) or small spatial scales (e.g., individual shoals). Especially at small spatial scales the transition in sediment composition may be abrupt (