How to identify Citrine
Quartz (SiO2) variety
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Open the appTo correctly identify Citrine (Quartz (SiO2) variety), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Ranges from pale yellow to golden yellow, orange-yellow, and brownish-orange. Natural citrine tends to be paler, while heat-treated amethyst often exhibits more intense orange or reddish-orange tones, sometimes with a reddish tint at the tips of crystals.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy).
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Smooth to conchoidal fracture surfaces. Crystalline texture when observed in aggregates or as individual crystals.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Typically forms as prismatic hexagonal crystals with pyramidal terminations. Can also be found as massive or granular aggregates. Often twinned (Dauphin, Brazil, Japan twins).
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None. Quartz lacks cleavage.
- 6
Geological Environment
The rock formation and setting where it occurs
Found in igneous rocks (granites, pegmatites), metamorphic rocks (gneisses, schists), and hydrothermal veins. Also occurs in alluvial deposits as detrital grains due to its resistance to weathering.
Key Facts
- Hardness
- 7 on the Mohs scale
- Specific Gravity
- 2.65 g/cm
- Crystal System
- Trigonal
- Color
- Yellow, golden yellow, orange-yellow, brownish-orange
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Fracture
- Conchoidal
- Cleavage
- None
- Composition
- Silicon dioxide (SiO2)
Physical characteristics
- Crystal Habit: Prismatic hexagonal crystals with pyramidal terminations, massive, granular
- Cleavage Type: None
- Fracture Type: Conchoidal
- Tenacity: Brittle
- Luster Type: Vitreous
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