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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
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Indian activity in Wikipedia
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 | Though this project is inactive, you can help with : Mfundo Vilakazi (random unreferenced BLP of the day for 7 Apr 2025 - provided by User:AnomieBOT/RandomPage via WP:RANDUNREF). |
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The current HKCOTW is Yuen Woo-ping . Please help improve it to featured article standard.
Every week, a Hong Kong-related topic, stub or nonexistent article is picked to be the HK Collaboration of the Week. The previous HKCOTW was Kowloon-Canton Railway - see improvements.
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Every week, a lacking Irish topic is picked to be the Irish Collaboration of the Week. |