How to identify Strawberry Quartz
Quartz (SiO2) with inclusions of goethite or hematite
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Open the appTo correctly identify Strawberry Quartz (Quartz (SiO2) with inclusions of goethite or hematite), 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
Pink to red, often with visible red, orange, or brown specks or needles of inclusions. The base quartz is typically colorless or milky.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy) on crystal faces and fractured surfaces.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Smooth to slightly granular depending on the size and distribution of inclusions. Can be massive or crystalline.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Typically occurs as massive aggregates or well-formed hexagonal prismatic crystals, often terminated. The inclusions are dispersed within these forms.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None. Quartz exhibits conchoidal fracture.
- 6
Geological Environment
The rock formation and setting where it occurs
Hydrothermal veins, pegmatites, and other silica-rich igneous or metamorphic environments. The presence of iron-rich fluids during quartz crystallization is crucial for the formation of the inclusions.
Key Facts
- Hardness
- 7 on the Mohs scale (due to the quartz matrix)
- Specific Gravity
- 2.65 - 2.66 (typical for quartz, inclusions may slightly alter this)
- Crystal System
- Trigonal
- Color
- Pink to red with iron oxide inclusions
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Fracture
- Conchoidal
- Cleavage
- None
- Composition
- Silicon dioxide (SiO2) with inclusions of hematite (Fe2O3) or goethite (FeO(OH))
Physical characteristics
- Crystal Habit: Prismatic, massive, granular
- Cleavage Type: None
- Fracture Type: Conchoidal
- Tenacity: Brittle
- Luster Type: Vitreous
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