Читать книгу Monument Future - Siegfried Siegesmund - Страница 38

Organic carbonate rock (shell limestone; bio-sparite / packstone). Colour: pinkish to yellowish with some variegations with evidence of shells of Bivalves (Chlamys). Mineral: calcite. Decay morphologies: surface erosion; sulphate skin formation. Geology: “Calcare di Finale Ligure” formation (lower 44Miocene) of post-orogenetic deposits of the “Bacino del Finalese”. Quarry: near Orco-Feglino, few kilometres north of Finale Ligure (Savona). Use: thick point chiseled slabs mainly employed for cladding (Università L. Bocconi, G. Pagano 1941, Milan; Palazzo del Toro, E. Lancia 1939, Milan).