Search results for " karst"

showing 10 items of 45 documents

Processi paleocarsici e geositi: il caso del “libeccio antico” nel distretto marmifero di Custonaci, Sicilia nord-occidentale

2016

Abstract The Upper Triassic strata that crops out along the northern slope of Monte Sparagio, in the Custonaci “marble” district in northwestern Sicily, show an extensive development of dissolution cavities with a very variable shape and dimensions. Several different types of dissolution morphologies can be differentiated from microkarst to giant caverns. The cavities are filled up by polychrome silts or calcite cements or, in the larger caverns, by collapse breccias. The matrix between the collapse breccias is a polychrome silt that gives rise to an attractive ornamental stone, quarried in the past with the name of “Libeccio Antico”. The diagenetic processes that have controlled the format…

Settore GEO/02 - Geologia Stratigrafica E Sedimentologicacarbonate platforms dissolution karst geosite Triassic Sicily
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Evaporites in Sicily: geological and karst features

2012

Settore GEO/04 - Geografia Fisica E GeomorfologiaEvaporites Sicily karst
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The "Paleorisorgenza" of the Monte Conca gypsum karst system (south-central Sicily)

2010

Settore GEO/04 - Geografia Fisica E GeomorfologiaGypsum karst systemSicily
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Surface denudation rate of gypsum in Sicily

2016

Studies on surface denudation rate of karst rocks were carried out for many years with different methods, although researches on limestones are much more numerous than those on gypsum. In Sicily the most large and complete Messinian evaporite succession of Gruppo Gessoso – Solfifero outcrops and since 1993-1994 surface denudation measurements were performed on different types of gypsum by the Micro-Erosion Meter (M.E.M.) method. MEM stations were placed on natural sites representing different lithological features of gypsum outcrops of the Island: 1) selenite gypsum with centimetre-sized crystals; 2) selenite gypsum with sub-centimetre crystals; 3) gypsum arenite; 4) microcrystalline gypsum…

Settore GEO/04 - Geografia Fisica E GeomorfologiaGypsum karst Sicily denudation rate
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Hypogenic caves in Sicily: a preliminary study of morphological and depositional features

2012

Settore GEO/04 - Geografia Fisica E GeomorfologiaHypogenic caves Sicily karst
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Flank Margin Caves In Telogenetic Limestones In Italy

2017

Almost 20% of Italy is characterized by the outcropping of carbonate massifs ranging in age from Cambrian to Quaternary. Coastal karst is present in many Italian regions: from North-East to South and West: the Gulf of Trieste, the Conero (South of Ancona, Marche), the Adriatic coast of Apulia including Gargano, Murge and Salento, Maratea in Basilicata, Cilento in Campania, Circeo and Gaeta in Latium, Argentario and Giannutri Island in Tuscany, the southernmost part of the Ligurian Alps, Palermo Mts., San Vito Lo Capo, Syracuse coast and Marettimo Island in Sicily, and, especially, in Sardinia, which has carbonate rocks touching the sea along the coast of Balai near Porto Torres, Capo Caccia…

Settore GEO/04 - Geografia Fisica E GeomorfologiaKarstsalt-fresh water mixing coastal karst cave geomorphology coastal uplift speleogenesis
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EXPLORATIONS AND DOCUMENTATION ON THE ATEPETACO KARST SYSTEM (HUEYTAMALCO, PUEBLA, MEXICO)

2013

Settore GEO/04 - Geografia Fisica E GeomorfologiaMexico Karst system Atepetaco
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KARST LANDSCAPES IN SICILY (SOUTHERN ITALY), WITH EXAMPLES OF SUSTAINABLE EXPLOITATION

2010

Settore GEO/04 - Geografia Fisica E GeomorfologiaSicily karst landforms Nature Reserves.
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Karst underground protection in Sicily (southern Italy), some examples from speleological natural reserves

2011

Settore GEO/04 - Geografia Fisica E GeomorfologiaSicily karst speleological natural reserves
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Secondary minerals from halite caves in the Atacama Desert (Chile)

2017

In the past 15 years several expeditions by French, American and especially Italian cavers have surveyed over 15 km of salt cave passages in the Cordillera de la Sal, close to San Pedro de Atacama village (Atacama Desert, Northern Chile). Over 50 caves have been explored up to now at an elevation around 2,500 m asl. These karst systems are characterized by in-cave temperature of around 17 °C and a relative humidity always very low, with a maximum of 15%. This extreme aridity is due to the severe conditions of the area with only a couple millimeters annual rainfall and several years without rain. Currently the rare precipitation events are enough to allow the dissolution of the salt rock and…

Settore GEO/06 - MineralogiaSettore GEO/04 - Geografia Fisica E GeomorfologiaKarstsalt karst sulphates halides speleothems minerogenesis
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