
mineral
Rhodolite Garnet
Magnesium Aluminum Silicate; formula: (Mg,Fe)3Al2(SiO4)3
Hardness: 7-7.5 (Mohs scale); Color: Rose-pink to raspberry-red or purplish-red; Luster: Vitreous (glassy); Crystal structure: Isometric (dodecahedral); Cleavage: None (conchoidal fracture); Specific Gravity: 3.7-3.9
- Hardness
- 7-7
- Color
- Rose-pink to raspberry-red or purplish-red
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7-7.5 (Mohs scale); Color: Rose-pink to raspberry-red or purplish-red; Luster: Vitreous (glassy); Crystal structure: Isometric (dodecahedral); Cleavage: None (conchoidal fracture); Specific Gravity: 3.7-3.9
Formation & geological history
Formed through regional metamorphism of clay-rich sedimentary rocks or in certain igneous environments. It is a varietal mix of Pyrope and Almandine garnet. Geological ages vary by deposit from Archean to Tertiary.
Uses & applications
Primarily used as a gemstone in jewelry (rings, pendants, earrings). Also historically used as an industrial abrasive due to its hardness, though gem-quality specimens like this are reserved for lapidary use.
Geological facts
The name 'Rhodolite' comes from the Greek word 'rhodon' meaning rose. Unlike many other red gemstones, it is rarely treated with heat or chemicals to enhance color. It was first identified in the United States in North Carolina in the late 1890s.
Field identification & locations
Identify in the field by its distinct purplish-red hue (lacking the brownish secondary tones of common almandine), high refractive index resulting in high brilliance, and lack of cleavage. Common locations include Sri Lanka, Tanzania, Madagascar, and Zimbabwe.
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