
mineral
Clear Quartz Crystal on Matrix
SiO2 (Silicon Dioxide)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Colorless/transparent with brownish matrix; Luster: Vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Colorless/transparent with brownish matrix
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Colorless/transparent with brownish matrix; Luster: Vitreous (glassy); Crystal structure: Hexagonal/Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
Formation & geological history
Formed through the crystallization of silica-rich solutions in hydrothermal veins or igneous pegmatites. This specimen likely developed in an open cavity or vug, allowing for the formation of distinct crystal faces.
Uses & applications
Used in electronics for its piezoelectric properties, glassmaking, optical instruments, jewelry, and widely collected as a metaphysical or decorative specimen.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Clear quartz is often called 'Rock Crystal.' It has been used since antiquity for carvings and crystal balls.
Field identification & locations
Identify in the field by its hexagonal crystal habit, lack of cleavage, and ability to scratch glass. Commonly found worldwide, with major deposits in Brazil and Arkansas, USA.
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Septarian Pebble
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