Karst in Slovenia

A. Mihevc; F. Gabrovšek; M. Knez; P. Kozel; J. Mulec; B. Otoničar; M. Petrič; T. Pipan; M. Prelovšek; T. Slabe; S. Šebela; N. Zupan Hajna

doi:10.21701/bolgeomin.127.1.006

Autores/as

A. Mihevc Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts
F. Gabrovšek Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts
M. Knez Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts
P. Kozel Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts
J. Mulec Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts
B. Otoničar Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts
M. Petrič Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts
T. Pipan Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts
M. Prelovšek Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts
T. Slabe Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts
S. Šebela Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts
N. Zupan Hajna Karst Research Institute, Research Centre of the Slovenian Academy of Sciences and Arts

DOI:

https://doi.org/10.21701/bolgeomin.127.1.006

Palabras clave:

Eslovenia, karst, Kras, paisaje, rocas carbonatadas

Resumen

El karst es un tipo de paisaje con características y fenómenos hidrológicos especiales tanto en superficie como subterráneos. Su principal característica es la disolución de las rocas carbonatadas por agua enriquecida con CO₂ como proceso morfológico dominante, movilización de la roca en forma de solución y drenaje subterráneo prevalente que forma cuevas. En lengua eslovena, kras significa una superficie rocosa y desnuda que se desarrolla en calizas o dolomías y también se utiliza como un topónimo. Es decir, la palabra karst se ha desarrollado a partir del nombre de la meseta Kras, que es el sitio clásico y de referencia para el paisaje kárstico.

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Citas

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