Rock Identifier
Tumbled Clear Quartz/Rock Crystal (Silicon Dioxide (SiO2)) — mineral
mineral

Tumbled Clear Quartz/Rock Crystal

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale); Color: Colorless to pale yellowish; Luster: Vitreous/Glassy; Crystal structure: Trigonal (hexagonal system); Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.

Hardness
7 (Mohs scale)
Color
Colorless to pale yellowish
Luster
Vitreous/Glassy
Identified More mineral
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Physical properties

Hardness: 7 (Mohs scale); Color: Colorless to pale yellowish; Luster: Vitreous/Glassy; Crystal structure: Trigonal (hexagonal system); Cleavage: None/Conchoidal fracture; Specific gravity: 2.65.

Formation & geological history

Formed primarily from hydrothermal solutions in igneous and metamorphic rocks. It can also form in sedimentary environments. Quartz is found in almost all geological ages.

Uses & applications

Extensively used in jewelry (as gemstones), electronics (piezoelectric properties), glassmaking, and alternative healing (rock crystal collecting).

Geological facts

Clear quartz is the most iconic type of quartz. It has been used historically for lens making and 'crystal balls'. It's known for its ability to convert mechanical stress into electrical voltage.

Field identification & locations

Identify by its hardness (will scratch glass), lack of bubbles (distinguishing it from man-made glass), and conchoidal fracture. Often found in vein deposits or weathered out into stream beds.