Search results for "Cave morphology"

showing 1 items of 1 documents

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
researchProduct