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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 wikiPageLength "729".
- Slush_flow wikiPageOutDegree "7".
- Slush_flow wikiPageRevisionID "629232092".
- Slush_flow wikiPageWikiLink Avalanche.
- Slush_flow wikiPageWikiLink Category:Avalanches.
- Slush_flow wikiPageWikiLink Iceland.
- Slush_flow wikiPageWikiLink Latitude.
- Slush_flow wikiPageWikiLink Norway.
- Slush_flow wikiPageWikiLink Snow_pack.
- Slush_flow wikiPageWikiLink Snowpack.
- Slush_flow wikiPageWikiLink Water.
- Slush_flow wikiPageWikiLinkText "Slush flow".
- Slush_flow hasPhotoCollection Slush_flow.
- Slush_flow wikiPageUsesTemplate Template:Reflist.
- Slush_flow subject Category:Avalanches.
- Slush_flow hypernym Avalanche.
- Slush_flow type Article.
- Slush_flow type Article.
- Slush_flow type Hazard.
- Slush_flow type Landslide.
- 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 sameAs 雪泥流.
- Slush_flow sameAs m.0gmgzw3.
- Slush_flow sameAs Q7542357.
- Slush_flow sameAs Q7542357.
- Slush_flow wasDerivedFrom Slush_flow?oldid=629232092.
- Slush_flow isPrimaryTopicOf Slush_flow.