At low tide in the Bristol Channel, the sea recedes significantly, exposing vast areas of mudflats and sandbanks. This phenomenon is due to the channel's unique topography and the high tidal range, which can exceed 14 meters. As a result, areas near the coasts of Wales and England, such as the Severn Estuary, can see the water retreating several miles, creating expansive landscapes that are typically underwater during high tide.
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