A methodology for locating the original quarries used for constructing historical buildings: application to Málaga Cathedral, Spain

• Published in: Engineering geology Vol. 54; no. 3; pp. 287 - 298
• Main Authors: Galán, E, Carretero, M.I, Mayoral, E
• Format: Journal Article
• Language: English
• Published: Amsterdam Elsevier B.V 01.10.1999; Elsevier
• Subjects: Applied sciences; Building structure; Buildings; Buildings. Public works; Construction (buildings and works); Exact sciences and technology; Limestone; Masonry structure; Materials; Methodology; Málaga Cathedral; Natural stones; Quarries location; Religious building; Sandstone; Types of buildings; Europe; Spain; Limestone; Methodology; Málaga Cathedral; Sandstone; Quarries location; Isotopic analysis; Church; Chemical analysis; Petrography; Stone masonry; Old building; Quarry; Mineral composition; Physical properties; Old document; Localization
• ISSN: 0013-7952; 1872-6917
• DOI: 10.1016/S0013-7952(99)00042-3

It is often necessary to locate the original quarry which supplied the stone for a particular historical building. This stones could be used for future restoration work and for testing in the laboratory (artificial aging tests, physical properties determination, control of the efficacy of conservation treatments, etc.). Generally, reviewing historical documentation gives information about the geographical setting of quarries and location of the stones in the monument, but this information needs to be proved by field and laboratory studies. The comparative study of stone from quarries and monuments should basically include the following: (1) mineralogical and petrographical studies; (2) the chemical analysis of major, minor and trace elements; (3)stable isotopes determinations; (4) physical properties of quarry materials and unweathered building stone (water absorption, ultrasound transmission velocity, porosity and porous system, density, bulk density, compressive strength, etc.). This methodology was applied to Málaga Cathedral stones represented in the main façade, towers, and the western zone of the terrace, which, according to historical literature, came from Almayate (Miocene–Pliocene limestones) and Cerro Coronado (Permotriassic sandstone) in Málaga. The conclusion of the comparative study carried out on quarries and building stones was consistent with the information available from the historical documentation.