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Halo de meteorización

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Foto de un canto de basalto con un halo de meteorización.

Se denomina halo de meteorización a una capa exterior meteorizada que se forma en ciertas rocas. El grosor del halo de meteorización varía dependiendo del alcance hacia el interior de la roca que haya tenido la oxidación de los minerales.[1]​

Referencias

  1. ↑ Laustela, M.; Egli, M.; Kääb, A. (2003). «Weathering rind measurements and relative age dating of rockglacier surfaces in crystalline regions of the Eastern Swiss Alps». En Phillips, M.; Springman, S.M.; Arenson, L.U., eds. Permafrost: Proceedings of the 8th International Conference on Permafrost, Zurich, Switzerland, 21-25 July 2003. p. 627-632. ISBN 90 5809 582 7. 
Esta página se editó por última vez el 7 ago 2019 a las 15:23.
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