Rock Identifier
Yellow Quartz (Citrine or Quartzite Pebble) (Silicon Dioxide (SiO2)) — mineral
mineral

Yellow Quartz (Citrine or Quartzite Pebble)

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale), Color: Yellow to brownish-orange, Luster: Vitreous/Waxy (tumbled), Crystal structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific gravity: 2.65

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Physical properties

Hardness: 7 (Mohs scale), Color: Yellow to brownish-orange, Luster: Vitreous/Waxy (tumbled), Crystal structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific gravity: 2.65

Formation & geological history

Formed through the crystallization of silica-rich fluids in hydrothermal veins or as a constituent of igneous and metamorphic rocks. This specific specimen appears to be a water-worn or tumbled river pebble.

Uses & applications

Used primarily in jewelry (as citrine), as a collector's specimen, or for spiritual/metaphysical purposes. Common quartz is also used in glassmaking and abrasives.

Geological facts

Naturally yellow quartz is quite rare; much of the yellow quartz sold commercially is actually heat-treated amethyst. When natural, the color is often caused by trace amounts of iron.

Field identification & locations

Identify in the field by its hardness (will scratch glass) and lack of cleavage. Commonly found in riverbeds, beaches, and mountainous regions worldwide. It is a very durable and stable mineral.