Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Jose Maria Calaforra"'
Publikováno v:
Travaux de l'Institut de Speologie Emile Racovitza, Vol 57, Iss 2018, Pp 35-48 (2018)
A totally new corrosion form has been recently observed inside the Natuturingam cave (better known as Puerto Princesa Underground River) in Palawan (Philippines): the guano holes. They consist of perfectly rounded holes, 4–5 cm wide and up to 10–
Externí odkaz:
https://doaj.org/article/f639be650bf049ca9fdea4c32c10f611
Publikováno v:
Geogaceta, Vol 76 (2024)
Los espeleotemas son una herramienta útil para investigar el clima del pasado. Sin embargo, la monitorización ambiental de la atmósfera de las cuevas es fundamental para una mejor interpretación de los resultados geoquímicos de estalagmitas. Est
Externí odkaz:
https://doaj.org/article/5b8a5a945e9c4132a95ba4baa54ebfc2
Publikováno v:
Travaux de l'Institut de Speologie Emile Racovitza, Vol 57, Iss q, Pp 35-47 (2019)
A totally new corrosion form has been recently observed inside the Natuturingam cave (better known as Puerto Princesa Underground River) in Palawan (Philippines): the guano holes. They consist of perfectly rounded holes, 4–5 cm wide and up to 10–
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doajarticles::0c1a84a679631bf1b4324237124be732
http://www.speotravaux.iser.ro/18/art02.pdf
http://www.speotravaux.iser.ro/18/art02.pdf
Autor:
Angel Fernandez-Cortes, Raul Perez-Lopez, Tamara Martin-Pozas, Soledad Cuezva, Jose Maria Calaforra, Sergio Sanchez-Moral
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
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Fluid migration along faults can be highly complex and spatially variable, with channelled flow along karstified structures of the vadose zone. One such example is Vapor cave, near the urban area of Alhama de Murcia, situated along a tectonically act
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7b85fd0f6fed3ec09e9538d44dd3f8b2
http://hdl.handle.net/10261/234265
http://hdl.handle.net/10261/234265
Autor:
Fernando Gázquez, Ana Monteserín, Christina Obert, Carsten Münker, Ángel Fernández-Cortés, José María Calaforra
Publikováno v:
Geosciences, Vol 12, Iss 4, p 144 (2022)
Subaqueous gypsum (CaSO4·2H2O) crystals are relatively common in epithermal systems where sulfide ore deposits are present. The Giant Geode of Pulpí (Almería, SE Spain) hosts some of the largest (up to 2 m in length) subaqueous gypsum crystals dis
Externí odkaz:
https://doaj.org/article/9632bfe077184f9c88851d5afdf8b411
Autor:
Andrés Ulloa, Fernando Gázquez, Aurelio Sanz-Arranz, Jesús Medina, Fernando Rull, José María Calaforra, Guillermo E. Alvarado, María Martínez, Geoffroy Avard, J. Maarten De Moor, Jo De Waele
Publikováno v:
International Journal of Speleology, Vol 47, Iss 2, Pp 229-246 (2018)
The caves of the Irazú volcano (Costa Rica), became accessible after the partial collapse of the NW sector of the Irazú volcano in 1994, offering the opportunity to investigate active minerogenetic processes in volcanic cave environments. We perfor
Externí odkaz:
https://doaj.org/article/392fa0f901cf4d2d9bf4a93b473a98d8
Publikováno v:
International Journal of Speleology, Vol 46, Iss 1, Pp 93-97 (2017)
During the 2011 speleological expedition to the Puerto Princesa Underground River (Palawan, Philippines) a drapery characterized by several close-to-horizontal ribs has been noticed. Even without sampling and analyzing its internal growth layers, a d
Externí odkaz:
https://doaj.org/article/27a5bac092c74a09a11410c4b67c57c4
Publikováno v:
Acta Carsologica, Vol 47, Iss 1 (2018)
Fascinating and fragile environments as are the underground estuaries, need to be studied, understood and protected for present and future generations. Even if wide and abundant bibliography related to tides and their behaviour with respect to the ex
Externí odkaz:
https://doaj.org/article/e4faf69630ac4ce181daf23e20dc2fb6
Publikováno v:
International Journal of Speleology, Vol 37, Iss 1, Pp 41-52 (2008)
Karst caves exhibit a wide range of hydrological and hydrochemical responses to infiltration events, due to their physical heterogeneity space and dynamic variability over time, and due to non-Gaussian inputs (rain) and outputs (discharge). This pape
Externí odkaz:
https://doaj.org/article/1818a57bb47644cfb239e1439d2f4f8c