らんでいりゅう

    noun (common) (futsuumeishi)
  1. turbidity current
Forms
  • らんでいりゅう
  • らんでいりゅう
Generated definitions (experimental)
  1. turbidity current
  2. 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.
    Turbidity currents are phenomena where sediment is transported at the sea floor.
Generated collocations (experimental)