 Individual locations in Antarctica include areas of the Allan Hills, the Queen Fabiola Mountains (the Yamato ice field there covers an area of and is the largest such structure), Scharffenberg-Botnen and the Sør Rondane Mountains.Blue-ice areas are regions where more snow is removed by sublimation or by wind than accumulates by precipitation or wind-driven transport, leading to the emergence of (blue) ice.In most of Antarctica, the net tendency is for snow to accumulate except in coastal Antarctica where melting occurs and blue-ice areas where sublimation dominates.