Fluorite forms as a late-crystallizing mineral in felsic igneous rocks typically through hydrothermal activity. It is particularly common in granitic pegmatites. It may occur as a vein deposit formed through hydrothermal activity particularly in limestones.

• Size: Approx. 4.5"
• Polished on one side
• Since these are made by Mother Nature herself, please allow variation in shapes, size, and shades of color