|Location is approximate, estimate based on other nearby localities.|
|Latitude & Longitude:||38° North , 3° West (est.)|
|Margin of Error:||~114km|
|Other regions containing this locality:||Iberian Peninsula|
|Name(s) in local language(s):||Volcanes del Campo de Calatrava, Ciudad Real, Castilla-La Mancha, España|
Zeolites in volcanic rocks.
Also high-Co (up to 1.7% Co) Mn mineralizations displaying a variety of morphologies: spring aprons and feeders, pisolitic beds, wad beds and tufa-like replacements of plants and plant debris. The spring apron deposits formed in close proximity to Pliocene volcanic rocks (alkaline basaltic lava flows and pyroclastics) belonging to the so-called Calatrava Volcanic Field (Crespo & Lunar, 1997).
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32 valid minerals.
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- A. Crespo & R. Lunar (1997): Terrestrial hot-spring Co-rich Mn mineralization in the Pliocene-Quaternary Calatrava Region (central Spain). Geological Society, London, Special Publications, vol. 119, 253-264.
- M. Calvo, G. Calvo Sevillano, J. Viñals and A. Sanz (2010): Presencia de Ettringita y Thaumasita en Vacuolas de los Basaltos del Campo de Calatrava (Ciudad Real). Macla 13, 53-54. [http://www.ehu.es/sem/macla_pdf/macla13/Macla13_053.pdf]