
sedimentary
Quartz Pebble
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: yellowish-tan to off-white due to iron oxide staining. Luster: vitreous to waxy/dull. Cleavage: none. Specific gravity: ~2.65.
- Hardness
- 7 on Mohs scale
- Color
- yellowish-tan to off-white due to iron oxide staining
- Luster
- vitreous to waxy/dull
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Physical properties
Hardness: 7 on Mohs scale. Color: yellowish-tan to off-white due to iron oxide staining. Luster: vitreous to waxy/dull. Cleavage: none. Specific gravity: ~2.65.
Formation & geological history
Formed through the erosion and weathering of quartz-bearing igneous, metamorphic, or sedimentary rocks. Streams, rivers, or beach waves smooth and round the fragment over long periods.
Uses & applications
Used primarily for decorative landscaping, aquariums, aggregate in construction, or personal keepsakes and rock collecting.
Geological facts
Quartz is one of the most abundant minerals on Earth's surface. Small stream-worn pebbles like this often acquire a yellowish or brownish patina due to iron staining from surrounding soil and groundwater.
Field identification & locations
Identified by its hardness (scratches glass), smooth water-worn surface, and microcrystalline or crystalline silica composition. Commonly found along riverbeds, beaches, and gravel deposits worldwide.
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