five

Scor

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data.europa2024-06-27 收录
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https://data.europa.eu/data/datasets/7585-schor?locale=en
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overgrown natural expansion of land located on the sea or stream, caused by the sedimentation of sand or clay particles as a result of the reduction in the flow rate. First, a “slick” is formed. If the slibbing is so high that only rarely flooding occurs, there is a bark.
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