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RM1775   Variscite
#1386
Palazuelo de las Cuevas, Zamora, Castilla y León, Spain

Specimen formed by a large group of aggregated nodules of variscite with concentric growths and apple green color. They are enclosed in a matrix with limonite. We can see the concentric structures in the natural fracture. Since its discovery in 1970, the Palazuelo de las Cuevas deposit became the "source" of variscite for the NW of the Iberian peninsula.

Size: 4.5 x 3.8 x 3.3 cm.
Found in ±1980's
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