Milky Quartz Geode or Druzy Quartz
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: White to translucent; Luster: Vitreous (glassy) to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & Geological History
Formed through the precipitation of silica-rich hydrothermal fluids in cavities or veins of host rocks. The white color is caused by microscopic fluid inclusions trapped during crystal growth.
Uses & Applications
Used in the production of glass, ceramics, and electronics (due to piezoelectric properties). Smaller specimens are popular for rock collecting and metaphysical uses.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz specifically gets its appearance from gas or liquid bubbles that were trapped as the crystal formed millions of years ago.
Field Identification & Locations
Identify in the field by its hardness (cannot be scratched by steel), glassy luster on fresh surfaces, and lack of cleavage. Often found in riverbeds or eroded out of sedimentary limestone formations.
Identified on: 5/15/2026
Mode: Standard