The lapiaz of Peña Cabarga (Cantabria). Genesis and signifiance of an original form

Authors

  • Juan Carlos García Codrón Universidad de Cantabria

DOI:

https://doi.org/10.18172/cig.972

Abstract

Gaudy cone and pinnacle karsts have been exhumed in many points of Northern Spain by open pit mining activities. Usually considered, without a real basis, as a "tropical climate" inheritance, these forms must be explained as result of iron and lead sulphides alteration in an environment with a conjunction of favourable conditions to karst processes in present-day.

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Published

23-05-2013

How to Cite

1.
García Codrón JC. The lapiaz of Peña Cabarga (Cantabria). Genesis and signifiance of an original form. CIG [Internet]. 2013 May 23 [cited 2023 Mar. 23];15:17-28. Available from: https://publicaciones.unirioja.es/ojs/index.php/cig/article/view/972

Issue

Vol. 15 (1989)

Section

Articles

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