- Firn
Firn is partially-compacted
névé , a type ofsnow that has been left over from past seasons and has been recrystallized into a substance denser than névé. It isice that is at an intermediate stage betweensnow and glacial ice. Firn has the appearance of wet sugar, but has a hardness that makes it extremely resistant to shovelling. It generally has a density greater than 550 kg/m³ and is often found underneath the snow that accumulates at the head of aglacier .Snowflake s are compressed under the weight of the overlying snowpack. Individualcrystal s near the melting point are semiliquid and slick, allowing them to glide along other crystal planes and to fill in the spaces between them, increasing the ice's density. Where the crystals touch they bond together, squeezing the air between them to the surface or into bubbles.In the summer months, the crystal metamorphosis can occur more rapidly because of water percolation between the crystals. By summer's end the result is firn.
The minimum altitude that firn accumulates on a glacier is called the "firn limit", "firn line" or "snowline".
References
* [http://vulcan.wr.usgs.gov/Glossary/Glaciers/glacier_terminology.html USGS Glossary of Selected Glacier and Related Terminology]
* [http://www.physicalgeography.net/fundamentals/10ae.html Fundamentals of Physical Geography]
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