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User:Commodore Sloat

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The current date and time is 8 April 2025 T 03:32 UTC.


"the people in charge of Wikipedia have closed the entrance and opened a discussion on her who does not seem that she is going to arrive nowhere." --google translate


Blue-ice area
Blue-ice areas are regions of Antarctica where the ice surface has a blue colour, contrasting with the more common white Antarctic surface. They form around 1% of the continent's ice area. Blue-ice areas typically form when the movement of both air and ice are obstructed by topographic obstacles such as mountains that emerge from the ice sheet, generating particular climatic conditions where the net snow accumulation is exceeded by wind-driven sublimation and snow transports. They are noted for being hard and flat, enabling their use as a runway, in addition to their stability. Ice of up to 2.7 million years in age has been extracted from blue-ice areas. There are also large numbers of meteorites accumulated on them, either from direct falls or having been transported from elsewhere by ice flow. This NASA photograph shows a blue-ice area in the Miller Range, with a meteorite.Photograph credit: Nina Lanza / NASA

Mr. Commodore Sloat, I have run into many great edits of yours. For exhibiting excellence and dedication, you deserve a salute and this barnstar.Kiyosaki 01:05, 17 November 2006 (UTC)


Welcome!

[edit]

Hello, Commodore Sloat, and welcome to Wikipedia! Thank you for your contributions. I hope you like the place and decide to stay. Here are a few good links for newcomers:

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