Cadalso de los Vidrios leucogranite ‘Blanco Cristal’: a widely used heritage stone from Spain

Author:

Freire-Lista David M.123ORCID,Fort Rafael1

Affiliation:

1. Instituto de Geociencias IGEO (CSIC, UCM) Spanish Research Council CSIC – Complutense University of Madrid UCM., C/Severo Ochoa 7. Edificio Entrepabellones 7 y 8. Ciudad Universitaria, 28040 Madrid, Spain

2. Centro de Geociências (CGeo). Rua Silvino Lima. Universidade de Coimbra – Polo II, 3030-790 Coimbra, Portugal

3. Trás-os-Montes e Alto Douro University (UTAD)., Quinta de Prados, 5001-801 Vila Real, Portugal

Abstract

AbstractCadalso de los Vidrios leucogranite is extracted from the Sierra de Guadarrama (Spanish Central System) under the trade name ‘Blanco Cristal’. It is a fine- to medium-grained, hypidiomorphic and equigranular building stone that has been used in many heritage buildings, such as the Villena Palace (1534). The current annual production of Cadalso de los Vidrios leucogranite is approximately 8000 m3, of which 40% is exported around the world. It has been used in places such as the Vieux-Port in Marseille (France), Cork International Airport (Ireland) and the Puri EXIM Bank of Jakarta (Indonesia) among others. It is currently being used in the construction of the iconic tower of Jesus Christ of the Sagrada Familia Basilica, in Barcelona (Spain). Cadalso de los Vidrios leucogranite Blanco Cristal has excellent petrophysical properties, a uniform colour and good resistance to thermal shock and freezing temperatures. These qualities make Blanco Cristal an ideal material for monuments and buildings.

Publisher

Geological Society of London

Subject

Geology,Ocean Engineering,Water Science and Technology

Reference46 articles.

1. Bellido F. , Mejías M. , Armendáriz M. & Reyes J. 2005. Estudio petrológico y geoquímico de los leucogranitos del sondeo de Cadalso de los Vidrios y de las zonas de alteración intersectadas. Proceedings of the V Congreso Ibérico de Geoquímica and IX Congreso de Geoquímica de España, 6. Biblioteca electrónica de la Diputación Provincial de Soria.

2. Brandebourger E. 1984. Les granitoïdes hercyniens tardifs de la Sierra de Guadarrama (Systeme Central Espagne) Petrographie et geochimie. PhD thesis, L'Institut National Polytechnique de Lorraine.

3. Introduction to stone in historic buildings: characterization and performance

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