
Mineral
Rhodonite
Rhodonite (Manganese Iron Magnesium Calcium Silicate) - (Mn,Fe,Mg,Ca)SiO3
Hardness: 5.5 to 6.5 Mohs scale; Color: Pink to rose-red with black manganese oxide inclusions (dendritic veins); Luster: Vitreous to pearly; Crystal Structure: Triclinic; Cleavage: Perfect in two directions; Specific Gravity: 3.5 to 3.7
- Hardness
- 5
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 5.5 to 6.5 Mohs scale; Color: Pink to rose-red with black manganese oxide inclusions (dendritic veins); Luster: Vitreous to pearly; Crystal Structure: Triclinic; Cleavage: Perfect in two directions; Specific Gravity: 3.5 to 3.7
Formation & geological history
Formed in manganese-rich metamorphic rocks, hydrothermal ores, or contact metamorphic deposits. It is often found associated with manganese oxides and other silicate minerals. Most deposits date back to various Precambrian or Paleozoic geological eras depending on location.
Uses & applications
Commonly used as a gemstone for cabochons, beads, and carvings. Also used as an ornamental stone in jewelry, architecture, and interior design. Historically, it was used as an ore of manganese in minor capacities.
Geological facts
The name is derived from the Greek word 'rhodon', meaning 'rose'. It is the state gemstone of Massachusetts, USA. Unlike Rhodochrosite, which is a carbonate and reacts to acid, Rhodonite is a silicate and does not. The black veins are caused by the oxidation of manganese.
Field identification & locations
Identify in the field by its distinct rose-pink color contrasted against black manganese veins and its relatively high hardness. Common locations include Russia (Urals), Australia, Brazil, Sweden, and the USA (New Jersey, Massachusetts). For collectors, the presence of 'pink and black' patterns is the primary diagnostic feature.
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