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- Slush_flow abstract "A slush flow is a type of snow avalanche that occurs when the snow pack becomes saturated with water. They most commonly occur at higher latitudes in the spring. Because of their high water content they can flow down gentle slopes of only a few degrees. They are a significant hazard in Norway and Iceland and are responsible for the deaths of dozens of people as well as the destruction of buildings and the closure of roads.".
- Slush_flow wikiPageID "31645155".
- Slush_flow wikiPageRevisionID "472438378".
- Slush_flow hasPhotoCollection Slush_flow.
- Slush_flow subject Category:Avalanches.
- Slush_flow type Abstraction100002137.
- Slush_flow type Avalanche107405137.
- Slush_flow type Avalanches.
- Slush_flow type ChangeOfLocation107311115.
- Slush_flow type Descent107363346.
- Slush_flow type Event100029378.
- Slush_flow type Happening107283608.
- Slush_flow type Movement107309781.
- Slush_flow type PsychologicalFeature100023100.
- Slush_flow type Slide107404944.
- Slush_flow type YagoPermanentlyLocatedEntity.
- Slush_flow comment "A slush flow is a type of snow avalanche that occurs when the snow pack becomes saturated with water. They most commonly occur at higher latitudes in the spring. Because of their high water content they can flow down gentle slopes of only a few degrees. They are a significant hazard in Norway and Iceland and are responsible for the deaths of dozens of people as well as the destruction of buildings and the closure of roads.".
- Slush_flow label "Slush flow".
- Slush_flow label "雪泥流".
- Slush_flow sameAs 雪泥流.
- Slush_flow sameAs m.0gmgzw3.
- Slush_flow sameAs Q7542357.
- Slush_flow sameAs Q7542357.
- Slush_flow sameAs Slush_flow.
- Slush_flow wasDerivedFrom Slush_flow?oldid=472438378.
- Slush_flow isPrimaryTopicOf Slush_flow.