
mineral
Rhodonite
Rhodonite (MnSiO3)
Hardness: 5.5-6 on Mohs scale. Color: Rose-pink to reddish-brown, often with black dendrites or veins of manganese oxide. Luster: Vitreous to pearly. Crystal structure: Triclinic. Cleavage: Perfect in two directions. Specific Gravity: 3.4-3.7.
- Hardness
- 5
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 5.5-6 on Mohs scale. Color: Rose-pink to reddish-brown, often with black dendrites or veins of manganese oxide. Luster: Vitreous to pearly. Crystal structure: Triclinic. Cleavage: Perfect in two directions. Specific Gravity: 3.4-3.7.
Formation & geological history
Rhodonite typically forms during metamorphism of manganese-rich sediments or in hydrothermal veins of manganese ore deposits. It is often associated with other manganese minerals. Geological age can vary widely depending on the specific deposit, ranging from Precambrian to Cenozoic.
Uses & applications
Commonly used as an ornamental stone, for carving, and particularly for beads and cabochons in jewelry. Higher quality, translucent material is highly prized. Also used occasionally for small decorative objects.
Geological facts
The name 'Rhodonite' comes from the Greek word 'rhodon', meaning 'rose', referring to its characteristic pink color. It is the state gem of Massachusetts, USA. Its distinctive pink color with black manganese oxide inclusions gives it a unique and recognizable appearance.
Field identification & locations
Can be identified in the field by its distinct rose-pink to reddish-brown color, often with characteristic black manganese oxide inclusions (dendritic patterns or veins). Its hardness can be tested with a steel file (it will scratch steel). Commonly found in mining regions worldwide, including the United States (Massachusetts, New Jersey), Sweden, Australia, Russia (Urals), Brazil, Canada, and Japan. Look for it in manganese ore deposits or areas that have undergone regional metamorphism with manganese-rich protoliths. For collectors, look for vibrant pink colors and interesting patterns of black inclusions; polished specimens highlight these features.
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