Search results for " Cave"

showing 10 items of 124 documents

Utilizzo di Sildenafil citrato nella prevenzione della fibrosi dei corpi cavernosi nella IPP e nell'invecchiamento.

2011

Sildenafil citratoIPPinvecchiamento.prevenzione della fibrosi dei corpi cavernosiSettore MED/24 - Urologia
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Sulfuric acid speleogenesis (SAS) close to the water table: Examples from southern France, Austria, and Sicily

2016

Caves formed by rising sulfuric waters have been described from all over the world in a wide variety of climate settings, from arid regions to mid-latitude and alpine areas. H2S is generally formed at depth by reduction of sulfates in the presence of hydrocarbons and is transported in solution through the deep aquifers. In tectonically disturbed areas major fractures eventually allow these H2S-bearing fluids to rise to the surface where oxidation processes can become active producing sulfuric acid. This extremely strong acid reacts with the carbonate bedrock creating caves, some of which are among the largest and most spectacular in the world. Production of sulfuric acid mostly occurs at or…

Speleogenesi010504 meteorology & atmospheric sciencesWater tableSettore GEO/04 - Geografia Fisica E GeomorfologiaGeochemistry[SDU.STU]Sciences of the Universe [physics]/Earth SciencesAquifer010502 geochemistry & geophysics01 natural scienceschemistry.chemical_compoundPaleontologyCaveSpeleogenesis0105 earth and related environmental sciencesEarth-Surface ProcessesCondensation-corrosiongeographygeography.geographical_feature_categoryHypogenic karstBedrockAuthigenicchemistry13. Climate actionSulfuric acid caveSubaerialCave morphologyCarbonateSulfuric acid caves Hypogenic karst Cave morphology Speleogenesis Condensation–corrosionGeology
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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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Morphology and evolution of sulphuric acid caves in South Italy

2016

Sulphuric acid speleogenesis (SAS) related to the upwelling of acid water enriched in H2S and CO2 represents an unusual way of cave development. Since meteoric infiltration waters are not necessarily involved in speleogenesis, caves can form without the typical associated karst expressions (i.e. dolines) at the surface. The main mechanism of sulphuric acid dissolution is the oxidation of H2S (Jones et al., 2015) which can be amplified by bacterial mediation (Engel et al., 2004). In these conditions, carbonate dissolution associated with gypsum replacement, is generally believed to be faster than the normal epigenic one (De Waele et al., 2016). In Italy several SAS caves have been identified…

Sulphuric acid cave speleogenesis HypogenicSettore GEO/04 - Geografia Fisica E Geomorfologia
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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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Water transfer from Basilicata to Puglia: a technical, economic and institutional challenge

2007

The necessity of supplying Puglia by transfer of water resources from Basilicata (250 Mm/year mainly for civil use but also for agricultural and industrial uses) and another bordering region (Campania for 200 Mm/year only for civil use) arises from the scarcity of water resources inside Puglia, where precipitation is very low (400 mm/year), rivers are few and with limited watersheds and costal aquifers are overexploited with salt intrusion. Moreover recent droughts have pointed out the need for revising water supply policy in Puglia, looking for the increment of the transfer of water resources from Basilicata (50 Mm/year) and Campania (32 Mm/year) and the development of feasibility studies …

Water resourcesWater transferEnvironmental protectionbusiness.industryAgriculturekarst cave sea levelEnvironmental scienceWater supplyWater industrybusinessEnvironmental planningWater Resources Management IV
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Understanding the Impact of Trampling on Rodent Bones

2022

Experiments based on the premise of uniformitarism are an effective tool to establish patterns of taphonomic processes acting either before, or after, burial. One process that has been extensively investigated experimentally is the impact of trampling to large mammal bones. Since trampling marks caused by sedimentary friction strongly mimic cut marks made by humans using stone tools during butchery, distinguishing the origin of such modifications is especially relevant to the study of human evolution. In contrast, damage resulting from trampling on small mammal fossil bones has received less attention, despite the fact that it may solve interesting problems relating to site formation proces…

Wonderwerk CaveBone compression[SHS.ARCHEO]Humanities and Social Sciences/Archaeology and PrehistoryMicrofaunaEarth and Planetary Sciences (miscellaneous)Experimental taphonomyPaleontologíaEarth-Surface Processes
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Investigation of marine and continental layers in a stalactite older than 1 million years (Custonaci, north-western sector of Sicily)

2012

Questo lavoro si basa sul ritrovamento, in una grotta carsica, a 100 metri di quota a Custonaci in provincia di Trapani, di una stalattite di notevole interesse paleo climatico, ricoperta da coralli marini, la cui sezione rivela la presenza di 3 Iatus che denotano una interruzione della deposizione di carbonato continentale presumibilmente in seguito a trasgressioni marine. Il carbonato, datato attraverso la metodologia 230Th/U MC-ICPMS (NeptunePlus), ha fornito una età più antica del limite temporale massimo di applicabilità del metodo ( 600 ka). I coralli, che ricoprono il livello continentale più giovane, analizzati usando il rapporto 87Sr/86Sr, hanno fornito una età di 1.1±0.2 Myrs. Al…

[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere[SDU.OCEAN] Sciences of the Universe [physics]/Ocean AtmosphereSettore GEO/04 - Geografia Fisica E GeomorfologiaSettore GEO/01 - Paleontologia E Paleoecologia[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environmentspeleothem with marine and continental layers coral overgrowth submerged cave.[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces environmentComputingMilieux_MISCELLANEOUS
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