A tidal flat forms in coastal areas where the land meets the sea, specifically in regions with significant tidal fluctuations. As tides rise and fall, sediment such as sand, silt, and clay is deposited during low tide, creating a flat, muddy area. Over time, these deposits accumulate and can be colonized by various plant and animal species, contributing to the ecosystem's biodiversity. Tidal flats are dynamic environments influenced by water movement, sediment supply, and ecological interactions.
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