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The Potential Geosite of the “Libeccio Antico” Quarries: a Sedimentological and Stratigraphic Characterisation of Ornamental Stone from Mt Cocuccio, Custonaci Marble District, Sicily

The Potential Geosite of the “Libeccio Antico” Quarries: a Sedimentological and Stratigraphic... The Custonaci marble district of western Sicily is known for the production of a valuable ornamental stone that has been, and nowadays is exploited due to its suitable properties and aesthetic qualities. The “Libeccio Antico” was, among the “marbles”, the most appreciated ornamental stone during the Baroque Age (the XVII–XVIII centuries), due to its strong polychrome contrasts from ivory to yellow, green or dark red. This polychrome pattern is the result of dissolution processes that involved an Upper Triassic peritidal limestone. The varicoloured sediments in paleocavities, collapse breccias, paleosols and neptunian dykes that occur in the “Libeccio Antico” represent the peculiar characteristics that have given this stone its particular ornamental interest. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Geoheritage Springer Journals

The Potential Geosite of the “Libeccio Antico” Quarries: a Sedimentological and Stratigraphic Characterisation of Ornamental Stone from Mt Cocuccio, Custonaci Marble District, Sicily

Geoheritage , Volume 11 (3) – Nov 20, 2018

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References (48)

Publisher
Springer Journals
Copyright
Copyright © 2018 by The European Association for Conservation of the Geological Heritage
Subject
Earth Sciences; Historical Geology; Physical Geography; Biogeosciences; Paleontology; Landscape/Regional and Urban Planning; Mineralogy
ISSN
1867-2477
eISSN
1867-2485
DOI
10.1007/s12371-018-0337-5
Publisher site
See Article on Publisher Site

Abstract

The Custonaci marble district of western Sicily is known for the production of a valuable ornamental stone that has been, and nowadays is exploited due to its suitable properties and aesthetic qualities. The “Libeccio Antico” was, among the “marbles”, the most appreciated ornamental stone during the Baroque Age (the XVII–XVIII centuries), due to its strong polychrome contrasts from ivory to yellow, green or dark red. This polychrome pattern is the result of dissolution processes that involved an Upper Triassic peritidal limestone. The varicoloured sediments in paleocavities, collapse breccias, paleosols and neptunian dykes that occur in the “Libeccio Antico” represent the peculiar characteristics that have given this stone its particular ornamental interest.

Journal

GeoheritageSpringer Journals

Published: Nov 20, 2018

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