Search results for "CAVE"

showing 10 items of 606 documents

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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Le cave sotterranee di Marsala (Sicilia occidentale) e i fenomeni di sprofondamento connessi

2014

Settore GEO/04 - Geografia Fisica E GeomorfologiaSettore GEO/05 - Geologia ApplicataMarsala Cave sotterranee Sprofondamenti calcarenite
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Caves in the Belmonte Mezzagno area (PA).

2009

Settore GEO/04 - Geografia Fisica E Geomorfologiacaves giant dormhouse Sicily
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Inside The Glaciers Project: Laser Scanning Of The Grotta Del Gelo (Mount Etna, Italy)

2017

As part of activities of the “Inside the Glaciers” project, managed by an Italian team of speleologists and geologists with the purpose of studying several ice-caves in Europe and South America, a research campaign was recently carried out in Mount Etna (Sicily, Italy). This volcano is the highest active in Europe and hosts more than 200 caves including Grotta del Gelo (Ice Cave) which is located on the Northern flank of Mount Etna at an altitude of about 2040 m a.s.l. This cave was formed during the Etna’s long and most destructive eruption dated from 1614 to 1624 and is one of the most famous because it hosts a small glacier, maybe the southernmost of the Northern hemisphere. Aim of this …

Settore GEO/04 - Geografia Fisica E Geomorfologiageomorphologyice caveLaser scanning; 3D modelling; ice caves; geomorphology; documentationdocumentationLaser scanning3D modelling
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Sprofondamenti di origine antropica nell'area di Marsala (Sicilia occidentale) analizzati mediante rilievi in sito e analisi numerica dei processi di…

2013

Settore GEO/04 - Geografia Fisica E Geomorfologiasprofondamenti cavità artificiali cave sotterranee modellazione numerica SiciliaSettore GEO/05 - Geologia Applicata
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Hypogenic caves of Sicily (Southern Italy)

2013

First results of a study on hypogenic caves in Sicily are presented. Inactive water-table sulphuric acid caves and 3D maze caves linked to rising of thermal waters rich in H2S were recognized. Cave patterns are guided by structural planes, medium and small scale morphological features are due mainly to condensation-corrosion processes. Calcite and gypsum represent the most common cave minerals. Different types of phosphates linked to the presence of large bat guano deposits were analyzed.

Settore GEO/06 - MineralogiaSpeleogenesisHypogenic caveSettore GEO/04 - Geografia Fisica E GeomorfologiaSicilyHYPOGENIC CAVES
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Secondary Minerals From Italian Sulfuric Acid Caves

2017

Italy is a country hosting a large number of hypogenic sulfuric acid (SAS) speleogenesis caves, mostly located along the Apennine chain, but also in Campania (along the coastline of Capo Palinuro), Apulia (along the coastline of Santa Cesarea Terme) and Sicily. Besides the typical morphologies related to their special geochemical origin (cupolas, replacement pockets, bubble trails, etc), these caves often host abundant secondary mineral deposits, mainly gypsum, being the result of the interaction between the sulfuric acid and the carbonate host rock. Native sulfur deposits are also well visible on the ceiling and roof, and peculiar sulfuric acid minerals such as jarosite, alunite, and other…

Settore GEO/06 - Mineralogiaspeleogenesihypogenic cavecave mineralogySettore GEO/04 - Geografia Fisica E Geomorfologiasulfate
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Architetture artificiali “per via di levare”. Una cava di calcarenite.

2020

Nel 1756, Pietro Bellaroto acquistò una chiusa di "terre scapole" nella Fossa della Garofala; questa gli fu poi alienata nel 1759 a favore di Giovanni Gerardi. Per tutto il XVII secolo il Bellaroto aveva iniziato a coltivare una cava di pietra (pirrera, dal termine spagnolo pedrera), la cui produzione lapidea venne utilizzata per la costruzione di molti edifici palermitani, intra ed extra moenia; la cava veniva chiamata pirrera di Bellaroto e la pietra prodotta era definita "forte", di buona qualità.

Settore ICAR/10 - Architettura Tecnicamateriali da costruzione tecniche costruttive materiali lapidei cave.
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Connettere frammentando

2009

Settore ICAR/14 - Composizione Architettonica E UrbanaAree di scavo cave progetto urbano
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A Pipeline for the Implementation of Immersive Experience in Cultural Heritage Sites in Sicily

2022

Modern digital technologies allow potentially to explore Cultural Heritage sites in immersive virtual environments. This is surely an advantage for the users that can better experiment and understand a specific site, also before a real visit. This specific approach has gained increasing attention during the extreme conditions of the recent COVID-19 pandemic. In this work, we present the processes that lead to the implementation of an immersive app for different kinds of low and high cost devices, which have been attained in the context of the 3dLab-Sicilia project. 3dLab-Sicilia’s main objective is to sponsor the creation, development, and validation of a sustainable infrastructure that int…

Settore ING-INF/05 - Sistemi Di Elaborazione Delle InformazioniVirtual heritageSettore INF/01 - InformaticaVR-headsetCultural heritageCAVEVirtual reality
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