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Variscite
Main Deposits
Specimens such as the one in the photo originate from Montcada i Reixac, Barcelona (Spain)
Description and Characteristics
Variscite is a hydrated aluminum phosphate formed by the deposition of phosphate-rich waters on aluminous rocks. It is a secondary mineral that usually appears as cryptocrystalline masses, nodules, or crusts; well-formed crystals are very rare. Its color ranges from pale green to deep emerald green, sometimes with bluish tints. Unlike turquoise, variscite owes its color primarily to chromium (rather than copper) and often features a white or grayish matrix of aluminum phosphates like wardite.
| Chemical Formula | $$AlPO_4·_2H_2O$$ |
|---|---|
| Luster | Waxy to vitreous |
| Streak | White |
| Fracture | Conchoidal to uneven |
| Cleavage | Poor |
| Hardness | 3.5-4.5 Mohs |
| Crystal System | Orthorhombic |
Did you know...?
It was first described in 1837 in the region of Variscia (Saxony, Germany), which gives it its name. In the United States, the Utah variety is extremely famous and is sometimes called "Utahlite." In Spain, there are very important prehistoric deposits, such as the Can Tintorer Mines in Gavá (Barcelona), where Neolithic people were already mining variscite to make beads and ornaments over 5,000 years ago.
New-Age Properties
Variscite is known as the "stone of calm" and hope. It is linked to the heart chakra, promoting a sense of deep peace and emotional clarity. It is said to help one move out of states of despair and find rational solutions to complex problems. It is an excellent stone for those suffering from stress or anxiety, as its gentle energy helps soothe the nervous system. Spiritually, it facilitates past-life recall and helps express feelings with honesty and simplicity.