Pharmacolite
Pharmacolite is a calcium arsenate hydrate mineral that forms as a secondary phase in oxidized zones of arsenic-rich environments. It typically crystallizes as small, tabular to platy crystals, often with a vitreous to pearly luster and a pale to colorless to light blue-green color that can be quite delicate. The mineral commonly occurs in association with other arsenates and phosphates, reflecting its formation under relatively dry, low-temperature conditions near hydrothermal or supergene environments. Chile is a well-known source for Pharmacolite specimens, where oxidized pockets and neuropathic arid terrains yield small, well-formed crystals that are prized by collectors for their subtle coloration and crystal habit. Collectors value Pharmacolite for its rarity in many localities and the challenge of finding well-preserved, sharp faces with clean termination, often showcased in small crystals within matrix or vug-like cavities.
- Formula
- Ca(HAsO4) · 2H2O
- Rarity
- Rare
- Stability
- Moderately Stable
- Collector interest
- Moderate Interest
About Pharmacolite
Overall, Pharmacolite appeals to collectors who seek delicate arsenate minerals with distinctive platy forms and gentle luster. Its connection to specific geochemical environments and limited, high-quality finds makes encountering representative specimens a noteworthy achievement for mineral enthusiasts and collection display. Proof of a mineral’s formation environment and its crystal habits contribute to its appeal, as does the quiet elegance of its pale hues when light passes through thin, translucent faces.