{"id":127,"date":"2026-06-11T11:32:43","date_gmt":"2026-06-11T11:32:43","guid":{"rendered":"https:\/\/palaciodelviso.com\/?p=127"},"modified":"2026-06-15T07:07:20","modified_gmt":"2026-06-15T07:07:20","slug":"geologia-del-palacio","status":"publish","type":"post","link":"https:\/\/palaciodelviso.com\/?p=127","title":{"rendered":"GEOLOG\u00cdA DEL PALACIO"},"content":{"rendered":"\n

PRINCIPALES ROCAS UTILIZADAS EN LA CONSTRUCCI\u00d3N DEL PALACIO:<\/p>\n\n\n\n

En el Palacio del Marqu\u00e9s de Santa Cruz<\/strong>, se utilizaron para su construcci\u00f3n: m\u00e1rmol<\/strong> (importado de Italia) en patios y zonas nobles, piedra caliza o arenisca local<\/strong> en canter\u00eda estructural, ladrillo<\/strong> y piedra rodada<\/strong> en muros, y pizarra<\/strong> en la escalera y suelos.<\/p>\n\n\n\n

La piedra rodada (cuarcita) y el ladrillo utilizados en la construcci\u00f3n fueron extra\u00eddos de canteras locales en el t\u00e9rmino de El Viso del Marqu\u00e9s. El m\u00e1rmol, por su parte, es de origen italiano, reflejando la influencia renacentista italiana en la decoraci\u00f3n del palacio. Esta elecci\u00f3n de materiales subraya el car\u00e1cter renacentista del edificio, fusionando lo local con lo importado para crear una obra arquitect\u00f3nica \u00fanica<\/strong>.<\/p>\n\n\n\n

M\u00e1rmol<\/strong>: Utilizado en las zonas m\u00e1s nobles del palacio, como el patio central, donde se encuentran arcadas de m\u00e1rmol con \u00f3rdenes d\u00f3rico y j\u00f3nico, y en las chimeneas interiores. Procedencia italiana.<\/p>\n\n\n\n

\"\"
Chimeneas con detalles en m\u00e1rmol<\/figcaption><\/figure>\n\n\n\n
\"\"<\/figure>\n\n\n\n

Canter\u00eda<\/strong>: Empleada en las esquinas y elementos estructurales destacados, como las pilastras del patio y las columnas de la escalera. Piedra de canter\u00eda<\/strong>: Es la piedra que ha sido cortada y labrada<\/strong> con herramientas para que tenga formas regulares (como bloques rectangulares), permitiendo su colocaci\u00f3n precisa en la construcci\u00f3n. En el caso del Palacio del Marqu\u00e9s de Santa Cruz<\/strong>, la canter\u00eda fue empleada para elementos estructurales y decorativos importantes, como las pilastras, columnas y molduras<\/strong>, dando solidez y elegancia al edificio.<\/p>\n\n\n\n

\"\"
Columna del patio<\/figcaption><\/figure>\n\n\n\n

En Viso del Marqu\u00e9s, las canteras hist\u00f3ricas se localizaron principalmente en las cercan\u00edas del municipio, aprovechando las formaciones geol\u00f3gicas predominantes en la regi\u00f3n. Seg\u00fan el mapa geol\u00f3gico<\/u><\/em> de Ciudad Real, la zona presenta una combinaci\u00f3n de dep\u00f3sitos hidrotermales y costras calc\u00e1reas, lo que sugiere la presencia de formaciones calc\u00e1reas aptas para la canter\u00eda (Caliza urbana).<\/p>\n\n\n\n

\"\"<\/figure>\n\n\n\n

Caliza Urbana. Kralodvoriense\/Ashgill inferior. A techo de los Bancos Mixtos aparece un tramo de rocas carbonatadas muy discontinuo, de espesor medio entre 5 y 20 m, conocido como Caliza Urbana (HENKE, 1926), la \u00fanica unidad propiamente calc\u00e1rea del Ordov\u00edcico de la Zona Centroib\u00e9rica. Su nombre est\u00e1 tomado de la terminolog\u00eda minera de Los Guindos (Ja\u00e9n), donde fue atravesada por el pozo Urbana.<\/em><\/p>\n\n\n\n

Aunque no se dispone de informaci\u00f3n espec\u00edfica sobre las canteras exactas utilizadas en la construcci\u00f3n del Palacio del Marqu\u00e9s de Santa Cruz, es probable que se emplearan piedras locales, como calizas<\/strong>, que son comunes en la regi\u00f3n y adecuadas para la talla y construcci\u00f3n. Adem\u00e1s, se sabe que en la zona se han explotado recursos como el cuarzo.<\/p>\n\n\n\n

En resumen, es razonable suponer que las piedras utilizadas en la canter\u00eda del palacio provienen de canteras locales, aprovechando los recursos geol\u00f3gicos disponibles en Viso del Marqu\u00e9s y sus alrededores.<\/p>\n\n\n\n

\"\"<\/figure>\n\n\n\n

Pizarra: <\/strong>Dado que Viso del Marqu\u00e9s se encuentra en la provincia de Ciudad Real, en Castilla-La Mancha, es posible que la pizarra utilizada en la construcci\u00f3n del Palacio del Marqu\u00e9s de Santa Cruz haya sido importada desde estas regiones productoras, como Valdeorras (Ourense), debido a la calidad y reputaci\u00f3n de la pizarra de esa zona. Sin embargo, sin informaci\u00f3n espec\u00edfica sobre las fuentes hist\u00f3ricas de la \u00e9poca, esta sigue siendo una suposici\u00f3n razonable.<\/p>\n\n\n\n

\"\"
Escalera de pizarra<\/figcaption><\/figure>\n\n\n\n
\"\"
Suelos de pizarra y m\u00e1rmol (restauraci\u00f3n s. XX)<\/figcaption><\/figure>\n\n\n\n

Obsidiana<\/strong>: es una roca \u00edgnea volc\u00e1nica que se forma por el enfriamiento r\u00e1pido de lava rica en s\u00edlice, y su presencia est\u00e1 asociada a zonas volc\u00e1nicas activas o recientes. En la Pen\u00ednsula Ib\u00e9rica, los yacimientos m\u00e1s conocidos se encuentran en \u00e1reas como las Islas Canarias, las Islas Baleares y algunas zonas del Pa\u00eds Vasco, pero no en la provincia de Ciudad Real. Por lo tanto, es poco probable que la obsidiana haya sido extra\u00edda localmente en Viso del Marqu\u00e9s. Si se ha encontrado obsidiana en la zona, es probable que haya sido importada desde regiones con yacimientos conocidos, como las mencionadas anteriormente.<\/p>\n\n\n\n

Sin embargo, en la provincia de Ciudad Real, existe una regi\u00f3n volc\u00e1nica conocida como el Campo de Calatrava<\/strong>, que abarca \u00e1reas como Ciudad Real, Almagro, Bola\u00f1os y Daimiel. Esta zona es una de las m\u00e1s importantes de la Pen\u00ednsula Ib\u00e9rica en t\u00e9rminos de vulcanismo reciente, con actividad que se desarroll\u00f3 entre hace 8,7 y 1,75 millones de a\u00f1os durante el Plioceno y el Cuaternario. El Campo de Calatrava incluye alrededor de 240 edificios volc\u00e1nicos diferenciados, siendo una de las tres zonas de vulcanismo reciente m\u00e1s relevantes de la pen\u00ednsula. En esta regi\u00f3n, el Basalto<\/strong> es una roca volc\u00e1nica com\u00fanmente utilizada en la construcci\u00f3n. Aunque Viso del Marqu\u00e9s no se encuentra directamente en el Campo de Calatrava, es posible que en \u00e9pocas pasadas se haya utilizado basalto proveniente de esta regi\u00f3n volc\u00e1nica cercana para la construcci\u00f3n de pavimentos o elementos arquitect\u00f3nicos. La proximidad de Viso del Marqu\u00e9s al Campo de Calatrava facilita el transporte de materiales desde las canteras volc\u00e1nicas de la zona. As\u00ed pues, aunque no se han identificado canteras de basalto en Viso del Marqu\u00e9s, la cercan\u00eda con el Campo de Calatrava sugiere que el basalto de esta regi\u00f3n volc\u00e1nica pudo haber sido utilizado en la construcci\u00f3n local, aprovechando su durabilidad y propiedades t\u00e9cnicas.<\/p>\n\n\n\n

RESUMEN<\/h2>\n\n\n\n

Rocas sedimentarias<\/u><\/strong><\/p>\n\n\n\n

    \n
  • Caliza<\/strong>: Muy usada por su facilidad para tallarla y su buena resistencia. De tipo \u00abCaliza urbana\u00bb, la encontramos en columnas, sillares de las esquinas, y varios elementos de adornos.<\/li>\n<\/ul>\n\n\n\n

    Rocas \u00edgneas<\/u><\/strong><\/p>\n\n\n\n

      \n
    • Basalto<\/strong>: Tambi\u00e9n muy resistente, aunque m\u00e1s oscura. Menos usada en detalles finos por su dureza. Lo encontramos en la plaza y alrededores de la iglesia.<\/li>\n\n\n\n
    • Obsidiana<\/strong>: vidrio volc\u00e1nico de color negro. Tambi\u00e9n la encontramos en la plaza.<\/li>\n<\/ul>\n\n\n\n

      Rocas metam\u00f3rficas<\/u><\/strong><\/p>\n\n\n\n

        \n
      • Pizarra<\/strong>: Utilizada sobre todo en cubiertas o pavimentos; es f\u00e1cil de dividir en l\u00e1minas.<\/li>\n<\/ul>\n\n\n\n
          \n
        • M\u00e1rmol<\/strong>: Muy apreciado por su belleza y capacidad de pulido. Se usa en escaleras, estatuas, columnas decorativas y revestimientos, balaustres y pasamanos. En el Palacio, detalles en las chimeneas del Sal\u00f3n de Honor.<\/li>\n<\/ul>\n\n\n\n

          <\/p>\n","protected":false},"excerpt":{"rendered":"

          PRINCIPALES ROCAS UTILIZADAS EN LA CONSTRUCCI\u00d3N DEL PALACIO: En el Palacio del Marqu\u00e9s de Santa Cruz, se utilizaron para su […]<\/p>\n","protected":false},"author":2,"featured_media":129,"comment_status":"open","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"categories":[31],"tags":[],"class_list":["post-127","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-explora-el-palacio"],"yoast_head":"\nGEOLOG\u00cdA DEL PALACIO - 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