El sistema de cuevas Snezhnaya-Mezhennogo-Illyuziya en el Cáucaso occidental

Autores/as

  • B.R. Mavlyudov Institute of Geography of the Russian Academy of Sciences

DOI:

https://doi.org/10.21701/bolgeomin.127.1.015

Palabras clave:

Cáucaso, geología, geomorfología, sedimentos de cueva, sistema de cuevas

Resumen


El sistema de cuevas Snezhnaya-Mezhennogo-Illyuziya (SMI) se encuentra en el macizo kárstico Khipstinsky, en el Cáucaso occidental. La cueva representa un sistema arborescente y ramificado de canales de cuevas a través de los que fluyen corrientes de agua subterránea y cambian en una dirección ascendente en pozos subverticales. Se han estudiado tres de dichos pozos que tienen una conexión con un río subterráneo: Snezhnaya (1 970 m s.n.m.), Mezhennogo (2 015 m s.n.m.) y Illyuziya (2 389 m s.n.m.). El sistema de cuevas SMI se investiga desde 1971 y la profundidad del sistema conocida hasta la fecha es de 1760 m, la longitud es de 32 km, el volumen es de 2.7 millones m3 y el volumen específico es 84 m3/m. La cámara más grande de la cueva, Thronnyj, tiene un tamaño de 309x109x40 m. La descarga media del río subterráneo es de 500 l/s. La temperatura en la cavidad varía de 0 a 6.5°C. La investigación del sistema de cuevas SMI continúa en la actualidad.

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Citas

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Publicado

2016-03-30

Cómo citar

Mavlyudov, B. (2016). El sistema de cuevas Snezhnaya-Mezhennogo-Illyuziya en el Cáucaso occidental. Boletín Geológico Y Minero, 127(1), 219–235. https://doi.org/10.21701/bolgeomin.127.1.015

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