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Transantarktiese Berge

Die blouys wat Fryxellmeer in die Transantarktiese Berge bedek, kom van die gletsersmeltwater van die Kanadagletser en ander kleiner gletsers. Die vars water bly bo-op die meer en vries en seel sodoende die pekelwater daaronder.

Die Transantarktiese Berge (85°00′S 175°00′W) is 'n bergreeks in Antarktika wat met 'n paar onderbrekings strek vanaf Kaap Adare tot Coats Land. Die berge dien as die skeiding tussen Oos-Antarktika en Wes-Antarktika. Ingesluit is die kontinue maar afsonderlik benoemde berggroepe langs die weste kant van die Rosssee en die westelike en suidelike kante van die Ross ysbank; so ook die Horlick Berge, die Thiel Berge, Pensacola berge, Shackleton Reeks en die Theron Berge. Die suiwer beskrywende naam is in 1962 deur US-ACAN aanbeveel en is sedertdien internasionaal aanvaar.

Kaart van die Transantarktiese Berge

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Transantarktiese Berge
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