Brandtite
6 in the gallery
Brandtite is a rare arsenate mineral with calcium, manganese, and arsenate groups in its structure. It typically forms as colorless to pale green crystals that can occur as elongated, prismatic aggregates with a vitreous to subadamantine luster. The mineral’s composition—Ca2Mn2+ (AsO4)2 · 2H2O—reflects its hydration and arsenate-bearing framework, and it often presents in microcrystalline to crystalline forms that are sought after by specialists. Distinguished specimens have come from localities in the United States and northern Europe, where secondary and metamorphic environments can promote its growth. The combination of delicate crystal habit, hydration, and arsenate chemistry makes Brandtite a standout among manganese- and calcium-bearing arsenates, attracting collectors who focus on rare, descriptor-rich constituents.
- Formula
- Ca2Mn2+(AsO4)2 · 2H2O
Where Brandtite is found
About Brandtite
Collectors prize Brandtite for its rarity and the elegance of its fine crystallization. While small, well-formed crystals or aesthetically pleasing aggregates can be exceptionally faceted and lustrous, the mineral’s scarcity means that well-documented specimens are prized for study and display. Localities in the USA and Germany or Sweden are noted for producing material that highlights the mineral’s distinctive formation conditions and mineralogical context, making Brandtite a meaningful addition to advanced mineral collections.

