How to identify Uvarovite Garnet
Ca3Cr2(SiO4)3
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Open the appTo correctly identify Uvarovite Garnet (Ca3Cr2(SiO4)3), 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
Vibrant emerald-green to dark green. The color is diagnostic for uvarovite among garnets.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy) to adamantine (diamond-like) when well-crystallized.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Typically forms as small, distinct crystals, often as a druzy coating or embedded in a matrix. Individual crystals are usually euhedral.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Cubic system, commonly forming dodecahedra or trapezohedra, or combinations thereof. Crystals are typically small, often less than a few millimeters.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None. Garnets are known for their lack of cleavage.
- 6
Geological Environment
The rock formation and setting where it occurs
Found in chromium-rich metamorphic rocks, particularly serpentinites, chromitites, and altered ultramafic rocks. Also occurs in skarns and hydrothermal veins associated with these environments.
Key Facts
- Hardness
- 6.5 - 7.5 on the Mohs scale
- Specific Gravity
- 3.41 - 3.85 (typically around 3.77)
- Crystal System
- Cubic
- Color
- Emerald-green to dark green
- Luster
- Vitreous to adamantine
- Transparency
- Transparent to translucent
- Fracture
- Conchoidal to uneven
- Cleavage
- None
- Composition
- Calcium chromium silicate
Physical characteristics
- Crystal Habit: Typically dodecahedral or trapezohedral crystals, often forming drusy coatings or embedded grains. Crystals are usually small, rarely exceeding a few millimeters.
- Cleavage Type: Absent (no cleavage)
- Fracture Type: Conchoidal to uneven
- Tenacity: Brittle
- Luster Type: Vitreous to adamantine
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