
mineral
Pink Chalcedony
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5–7 on Mohs scale. Color: Pale pink to dusty rose. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (Trigonal/Monoclinic). Cleavage: None. Specific gravity: 2.6–2.64.
- Hardness
- 6
- Color
- Pale pink to dusty rose
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5–7 on Mohs scale. Color: Pale pink to dusty rose. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (Trigonal/Monoclinic). Cleavage: None. Specific gravity: 2.6–2.64.
Formation & geological history
Formed through the deposition of silica from hydrothermal fluids in volcanic rocks or sedimentary environments. It often fills cavities (gas bubbles) or cracks in host rocks.
Uses & applications
Primarily used in jewelry making for cabochons and beads, as well as for ornamental carvings and lapidary practice. Also popular in metaphysical and crystal collecting communities.
Geological facts
Chalcedony is a cryptocrystalline form of silica, meaning its crystals are too small to be seen with a standard microscope. The pink hue is often attributed to trace amounts of manganese or microscopic inclusions of other minerals.
Field identification & locations
Identify in the field by its waxy luster, conchoidal (shell-like) fracture, and the fact that it can scratch glass but cannot be scratched by a steel knife. Commonly found in desert regions, particularly in the western United States, Brazil, and Namibia.
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