
mineral
Yellow Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Yellow to golden-orange due to iron oxide staining. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Yellow to golden-orange due to iron oxide staining
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale. Color: Yellow to golden-orange due to iron oxide staining. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
Formation & geological history
Formed in igneous or metamorphic hydrothermal veins as clear quartz, then eroded and water-worn in riverbeds or coastal environments. Stained yellow over time by micro-inclusions of iron oxides (hematite/goethite).
Uses & applications
Commonly collected as river rocks, used in landscaping, tumbling for lapidary hobbies, and occasionally made into beads or wire-wrapped jewelry.
Geological facts
Yellow quartz pebbles are often referred to as 'iron-stained quartz' or naturally stained quartzite. Despite their yellow hue, they are distinct from true citrine, which is colored by iron at the atomic lattice level rather than surface/fracture staining.
Field identification & locations
Identified in the field by its hardness (scratches glass, cannot be scratched by a steel knife), rounded water-worn shape, translucency, and yellow-orange iron staining within internal fractures. Extremely abundant in gravel bars, beaches, and riverbeds globally.
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Pegmatite with Tourmaline and Quartz
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Granite
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Septarian Pebble
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