por José Ignacio Canudo | 25/06/2023
Clinoclasa del Collado de la Plata, Albarracín. Foto Miguel Ángel Martínez
La clinoclasa es un raro mineral de alteración (Arsenato) que se forma en la zonas de oxidación de minerales hidrotermales con arsénico y cobre. Su color más habitual es azul o verde. Inicialmente se describió en Inglaterra, pero luego ha sido citado en minas por todo el mundo.
REFERENCIAS
Wikipedia / Asturnatura /
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