Search results for " caves"

showing 7 items of 27 documents

Sulfuric acid caves of Italy: A review

2019

Abstract In Italy, especially along the Apennine Chain, numerous active and inactive sulfuric acid speleogenetic (SAS) caves have been documented in the last two decades. Here we present an overview of these peculiar hypogene systems, illustrating their main geomorphological and mineralogical features, and the microbial signatures observed in the active underground environment. SAS caves are widely distributed in the northern and central Apennines, whereas they are less abundant in the southern Apennines, in the Apulian foreland, in Sicily and in Sardinia. Their location is significantly influenced by lithological and structural rock properties, as they occur in carbonate areas where acidic…

SpeleogenesigeographyCave sulfategeography.geographical_feature_category010504 meteorology & atmospheric sciencesEvaporiteHypogeneSettore GEO/04 - Geografia Fisica E GeomorfologiaGeochemistryKarst010502 geochemistry & geophysicsKarstAlunite01 natural scienceschemistry.chemical_compoundHypogene caveCavechemistryCarbonateSpeleogenesisHypogene caves Speleogenesis Karst Cave sulfatesForeland basinGeology0105 earth and related environmental sciencesEarth-Surface Processes
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A review on hypogene caves in Italy

2014

Although hypogene cave systems have been described since the beginning of the 20th century, the importance in speleogenesis of ascending fluids that acquired their aggressiveness from in-depth sources has been fully realized only in the last decades. Aggressiveness of waters can be related to carbonic and sulfuric acids and the related corrosion-dissolution processes give rise to different types of caves and underground morphologies. The abundance of hydrothermal springs and associated travertine deposits, and the widespread interaction between volcanic or sub-volcanic phenomena and karst in many sectors of the Italian peninsula are a strong evidence of hypogene speleogenesis. Furthermore, …

SpeleogenesisHypogene caveItalySettore GEO/04 - Geografia Fisica E Geomorfologiahypogene caves
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Sulfuric acid water table caves (Grotte du Chat / Acqua Fitusa /Bad Deutsch Altenburg + Kraushöhle).

2014

Sulfuric acid caves can display a variety of forms, from 3D maze systems, to isolated chambers, and more or less maze-like water table caves. Most of the voids are normally generated at or immediately above the water table, where condensation-corrosion processes are dominant, creating a set of characteristic meso- and micromorphologies. This paper deals with the description of four very typical sulfuric acid water table caves: the Grotte du Chat in Provence (France), the Acqua Fitusa Cave in Sicily (Italy), and the Bad Deutsch Altenburg and Kraushöhle caves in Austria.

Sulfuric acid cavesHypogenic caveSettore GEO/04 - Geografia Fisica E GeomorfologiaGeomorphologyHYPOGENIC CAVES
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The Complex of tectonic caves of the Vallone di Margi Paolino (Valle Grovello) area - Sant'Angelo Muxaro (AG).

2010

Tectonic caveSettore GEO/04 - Geografia Fisica E GeomorfologiaNatural ReserveTectonic caves gypsum Natural Reservegypsum
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Some Considerations on 3-D and 2-D Numerical Models for the Assessment of the Stability of Underground Caves

2014

The application of numerical modeling to the analysis of the stability of both natural and man-made underground caves is rapidly increasing due to the availability of powerful numerical codes, that can account for either continuum or discontinuum behavior of the rock masses. Numerical methods allow to overcome traditional methods for cave stability analysis that assume too simplified geometrical, geological and geomechanical conditions. Further, they are also able to assess the potential failure mechanisms of underground systems. On the other hand, the application of numerical methods requires availability of a detailed geo-structural survey of the cave, as well as a proper geomechanical ch…

geographyEngineeringgeography.geographical_feature_categorybusiness.industrySettore GEO/04 - Geografia Fisica E GeomorfologiaSinkholeUnderground caves Stability FEM model Three-dimensionalityCivil engineeringFinite element methodCalcareniteComplex geometryCaveGeotechnical engineeringRock mass classificationbusinessSettore GEO/05 - Geologia ApplicataJoint (geology)Plane stress
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Aerobiology: an ecological indicator for early detection and control of fungal outbreaks in caves

2011

5 pages, 1 table, 13 references.

medicine.medical_specialty[SDV]Life Sciences [q-bio]General Decision SciencesEarly detectionAerobiologyFungal outbreaks010501 environmental sciencesBiology01 natural sciencesAerobiology03 medical and health sciencesCavemedicineEcology Evolution Behavior and SystematicsComputingMilieux_MISCELLANEOUS[SDV.MP.MYC]Life Sciences [q-bio]/Microbiology and Parasitology/Mycology030304 developmental biology0105 earth and related environmental sciences0303 health sciencesgeographygeography.geographical_feature_categoryEcologyEcologyFungiOutbreaksocial sciencesmusculoskeletal systembiodiversity and conservationHazard[SDV.MP.MYC] Life Sciences [q-bio]/Microbiology and Parasitology/Mycologyhumanities3. Good health[SDE.BE] Environmental Sciences/Biodiversity and EcologyShow cavesEcological indicatorDisturbance (ecology)environmental sciences and ecologyThreatened species[SDE]Environmental Sciences[SDE.BE]Environmental Sciences/Biodiversity and Ecology
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Guano-related phosphate-rich minerals in European caves

2019

International audience; Guano is a typical deposit found in caves derived from the excretions of bats and in minor cases of birds. These organic deposits decompose and form a series of acid fluids and gases that can interact with the minerals, sediments, and rocks present in the cave. Over sixty phosphates are known and described from caves, but guano decay also often leads to the formation of nitrates and sulfates. In this study twenty-two European caves were investigated for their guano-related secondary minerals. Using various analytical techniques, seventeen phosphates, along with one sulfate (gypsum), were recognized as secondary products of guano decay. Among those minerals, some are …

phosphatesGypsum010504 meteorology & atmospheric sciencesQH301-705.5Settore GEO/04 - Geografia Fisica E GeomorfologiaGeochemistrybat guanocave minerals phosphate bat guanoengineering.material010502 geochemistry & geophysics01 natural sciencessecondary cave mineralsApatitechemistry.chemical_compoundCavesecondary cave minerals phosphates minerogenesis limestone caves bat guanominerogenesisBiology (General)Sulfatelimestone cavephosphate0105 earth and related environmental sciencesEarth-Surface Processescave mineralsQE1-996.5geographygeography.geographical_feature_categoryMineralSettore GEO/07 - Petrologia E PetrografiaGeology15. Life on landPhosphatehumanitiessecondary cave mineralchemistryminerogenesivisual_artlimestone cavesGuanoengineeringvisual_art.visual_art_mediumPyrite[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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