Quartz after Fluorite

This specimen features a grouping of sharp quartz epimorphs that have formed after what is believed to have been fluorite, displaying some sharply defined octahedral forms. The quartz formations are hollow, as evident from the incomplete crystals, which offer a fascinating glimpse into the mineral’s unique growth process.

The specimen was collected during a trip to a locality known as Gringo Gulch, near Patagonia, Arizona. This area is known for its distinctive mineral occurrences, particularly for amethyst crystals and now for these intriguing quartz epimorphs. For a detailed account of the collecting trip and more information on this locality, you can read the full story of our discovery here: Collecting Quartz Epimorphs Near Patagonia, AZ. (https://djoyceminerals.com/activities/collecting-quartz-epimorphs-near-patagonia-az/)