Lingaku- turbidity current
noun (common) (futsuumeishi)
Forms
Generated definitions (experimental)
- turbidity current
This term refers to a type of underwater current that is caused by the movement of sediment-laden water down the slope of the sea floor, often occurring in deep-sea environments. It is used in geological and oceanographic contexts.
Generated collocations (experimental)
らんでいりゅう乱泥流がはっせい発生するturbidity current occursらんでいりゅう乱泥流をかんそく観測するto observe a turbidity currentかいてい海底らんでいりゅう乱泥流submarine turbidity currentらんでいりゅう乱泥流のえいきょう影響impact of turbidity currentらんでいりゅう乱泥流のちょうさ調査study of turbidity currentえんがん沿岸らんでいりゅう乱泥流coastal turbidity currentらんでいりゅう乱泥流のめかにずむメカニズムmechanism of turbidity currentらんでいりゅう乱泥流にたいする対するたいさく対策measures against turbidity currentらんでいりゅう乱泥流のよそく予測prediction of turbidity currentらんでいりゅう乱泥流によるどしゃさいがい土砂災害sediment disaster caused by turbidity current