Quartz Geode Fragment
Silicon Dioxide (SiO2)
Rock Type: sedimentary

Physical Properties
Hardness: 7 on Mohs scale; Color: White to translucent crystals on brown host rock; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture).
Formation & Geological History
Formed as secondary mineral growth within hollow cavities of sedimentary or volcanic rocks. Mineral-rich groundwater seeps into voids, precipitating silica over millions of years.
Uses & Applications
Primarily used for geological education, home decor, and metaphysical collections. Industrial quartz is used in electronics and glassmaking.
Geological Facts
The word geode comes from the Greek word 'Geoides' meaning earth-like. Unlike a solid nodule, a true geode must have a hollow interior, though fragments like this represent the crystal wall.
Field Identification & Locations
Identify in the field by looking for rounded, bumpy 'nodules' that feel lighter than they look. Found commonly in limestone or shale beds in states like Iowa, Indiana, or in desert regions.
Identified on: 4/25/2026
Mode: Standard