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Lago subglaciar

De Wikipedia, la enciclopedia libre

Fotografía de dos lagos subglaciales de la Antártida realizada por la NASA.

Un lago subglacial es un lago que se halla permanentemente cubierto de hielo. Pueden presentarse debajo de glaciares y casquetes de hielo. Existen numerosos lagos subglaciales, siendo el Lago Vostok, en la Antártida, de lejos el más extenso con una superficie de unos 15.000 km².[1]​

El agua bajo el hielo permanece líquida debido a la presión de la fría capa sobre ella y al calor geotérmico.

El más reciente hallado ha sido el Lago CECs por el Centro de Estudios Científicos de Valdivia, Chile.

Referencias

  1. ↑ Gargaud, Muriel (2011). Encyclopedia of Astrobiology (en inglés). Springer. p. 1754. ISBN 3642112714. 

Enlaces externos

Esta página se editó por última vez el 6 mar 2022 a las 13:23.
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