Quartz and Dolomite on Fluorite

This complex mineral association formed in hydrothermal veins, where fluorite crystallized first within open cavities, later followed by dolomite and quartz deposited during successive stages of mineralization. The Wölsendorf district is a classic German fluorite locality, known for producing richly associated hydrothermal specimens.

The contrast of glassy quartz and soft dolomite atop geometric fluorite reflects the layered sequence of crystal growth, preserving multiple phases of mineral formation within one elegant specimen.