Summary
A comprehensive analysis of the petrographic, petrophysical, and engineering geological properties of stone materials used in the Late Baroque Towns of Val di Noto reveals a unique relationship between local geology and architectural innovation. The study identifies two primary lithotypes—Hyblean limestones (sedimentary) and Etnean lavas (magmatic)—whose distinct characteristics contribute to the towns' bichromy, a hallmark of their post-1693 earthquake reconstruction. Findings highlight how these stones, exposed to atmospheric agents like rain, freeze-thaw cycles, and saline crystallization, undergo weathering processes that threaten their durability. The research provides critical insights into the petrophysical behavior—including porosity, seismic resistance, and deterioration patterns—of these materials, offering a foundational tool for conserving and restoring this UNESCO-listed heritage. Published in Boletín Geológico Y Minero, this work bridges geological science and cultural preservation, emphasizing the importance of material properties in sustaining architectural integrity.
Citation
Punturo, R., Indelicato, V., Mineo, S., Pappalardo, G., Lanzafame, G., Visalli, R., & Cirrincione, R. (2026). Petrographic, petrophysical and engineering geological properties of stone materials employed in the Late Baroque of Val di Noto UNESCO Heritage sites (Sicily, Italy). Boletín Geológico Y Minero, 137(1), 3. https://doi.org/10.21701/bolgeomin/137.1/003