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- Melt-Freeze_Crust abstract "A Melt-Freeze Crust or Rain Crust is a discontinuity between snow layers which can lead to avalanches. The layer can be created in two ways:A temperature high enough to allow surface snow to melt, creating a layer of melt water which may later re-freeze. Rain falling and freezing on the surface of existing snow, also creating a frozen layer. This layer is brittle, smooth and slippery, and does not bond with snow layers above it, allowing the overlying slab of snow to move down the mountain under gravity when disturbed or if the accumulated snowfall exceeds a critical mass. The initial slab may be as large as 10,000m² and 10 metres thick.".
- Melt-Freeze_Crust wikiPageID "4999164".
- Melt-Freeze_Crust wikiPageLength "792".
- Melt-Freeze_Crust wikiPageOutDegree "4".
- Melt-Freeze_Crust wikiPageRevisionID "623118758".
- Melt-Freeze_Crust wikiPageWikiLink Avalanche.
- Melt-Freeze_Crust wikiPageWikiLink Category:Snow.
- Melt-Freeze_Crust wikiPageWikiLink Gravity.
- Melt-Freeze_Crust wikiPageWikiLink Snow.
- Melt-Freeze_Crust wikiPageWikiLinkText "Melt-Freeze Crust".
- Melt-Freeze_Crust wikiPageWikiLinkText "melt-freeze crust".
- Melt-Freeze_Crust wikiPageUsesTemplate Template:Reflist.
- Melt-Freeze_Crust subject Category:Snow.
- Melt-Freeze_Crust hypernym Discontinuity.
- Melt-Freeze_Crust type Disease.
- Melt-Freeze_Crust comment "A Melt-Freeze Crust or Rain Crust is a discontinuity between snow layers which can lead to avalanches. The layer can be created in two ways:A temperature high enough to allow surface snow to melt, creating a layer of melt water which may later re-freeze. Rain falling and freezing on the surface of existing snow, also creating a frozen layer.".
- Melt-Freeze_Crust label "Melt-Freeze Crust".
- Melt-Freeze_Crust sameAs Q16928635.
- Melt-Freeze_Crust sameAs m.0cz5xh.
- Melt-Freeze_Crust sameAs Q16928635.
- Melt-Freeze_Crust wasDerivedFrom Melt-Freeze_Crust?oldid=623118758.
- Melt-Freeze_Crust isPrimaryTopicOf Melt-Freeze_Crust.