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The soil in intertidal zones is typically composed of a mix of sand, silt, clay, and organic materials, resulting in a sedimentary type known as estuarine or marine sediment. This soil is often characterized by its high moisture content and variable salinity due to tidal influences. Additionally, it may contain a significant amount of nutrients, supporting diverse plant and animal life adapted to the fluctuating conditions of these zones. The texture can vary widely, from fine muds in quieter areas to coarser sands in more exposed locations.

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