Névé // is a young, granular type of snow which has been partially melted, refrozen and compacted, yet precedes the form of ice. This type of snow is associated with glacier formation through the process of nivation. Névé that survives a full season of ablation turns into firn, which is both older and slightly denser. Firn eventually becomes glacial ice – the long-lived, compacted ice that glaciers are composed of. Glacier formation can take days to years depending on freeze-thaw factors. Névé is annually observed in skiing slopes, and is generally disliked as an icy falling zone.
Névé can also refer to the alpine region in which snowfall accumulates, becomes névé, and feeds a glacier.
||This article includes a list of references, related reading or external links, but its sources remain unclear because it lacks inline citations. (June 2016) (Learn how and when to remove this template message)|
|This glaciology article is a stub. You can help Wikipedia by expanding it.|