How to identify Spessartine
Spessartine
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Open the appTo correctly identify Spessartine (Spessartine), 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
Orange, reddish-orange, yellowish-orange, brownish-red. The most prized specimens are vivid orange ('mandarin orange').
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy) to resinous.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Typically smooth on crystal faces, granular in massive forms.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Commonly forms well-developed dodecahedral (12-sided) or trapezohedral (24-sided) crystals. Also found as anhedral grains or massive aggregates.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None (garnets exhibit no true cleavage due to their isometric crystal structure).
- 6
Geological Environment
The rock formation and setting where it occurs
Manganese-rich metamorphic rocks (schists, quartzites, gneisses), granitic pegmatites, and sometimes in rhyolites and other acidic igneous rocks.
Key Facts
- Hardness
- 6.5-7.5 (Mohs scale)
- Specific Gravity
- 4.12-4.20 g/cm3
- Crystal System
- Isometric (Cubic)
- Color
- Orange, reddish-orange, yellowish-orange, brownish-red
- Luster
- Vitreous to resinous
- Transparency
- Transparent to translucent to opaque
- Fracture
- Conchoidal to uneven
- Cleavage
- None
- Composition
- Manganese Aluminum Silicate
Physical characteristics
- Crystal Habit: Typically dodecahedral or trapezohedral crystals; also granular, massive, or anhedral.
- Cleavage Type: None (parting may occur along lamellar twinning planes, but this is not true cleavage).
- Fracture Type: Conchoidal to uneven.
- Tenacity: Brittle.
- Luster Type: Vitreous (glassy) to resinous.
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