Strandflat is a geological term that refers to a coastal landform characterized by a flat or gently sloping beach or shore. This type of terrain is often found in regions where the shoreline has been shaped by various processes, including wave action, sediment deposition, and erosion. Strandflats are typically formed in areas with low relief and can result from the interaction between sea level changes and coastal processes. They may consist of a beach area that is broader and flatter compared to more rugged coastal formations.
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