Rhodonite beads (possibly dyed or treated, or lower quality Rhodonite)

Hardness: 5.5-6.5 (Mohs); Color: Rose-pink to red, often with black manganese oxide inclusions (visible in some beads); Luster: Vitreous to pearly; Crystal structure: Triclinic; Cleavage: Perfect on two directions; Specific Gravity: 3.4-3.7. The beads shown are tumbled and polished, minimizing visibility of crystal structure and cleavage, but the color is characteristic.

Rhodonite typically forms in metamorphic rocks under high-temperature and high-pressure conditions, often associated with manganese deposits. It can also occur in veins. Geological Age: Varies depending on the specific deposit, found in various geological eras.

Primarily used as an ornamental stone, particularly in jewelry (cabochons, beads, carvings). Also used for small sculptures and inlay work. The beads pictured are clearly for jewelry making.

Rhodonite is named from the Greek word 'rhodon', meaning 'rose', due to its distinctive pink to red color. It is sometimes confused with Rhodochrosite, but Rhodonite is harder and lacks the characteristic banding of Rhodochrosite. The presence of black veins or spots (manganese oxides) is common and often considered a desirable aesthetic feature in rhodonite. Some rhodonite on the market is dyed to enhance its pink-red color, especially if the natural coloration is paler.

In the field, rhodonite can be identified by its distinctive pink/red color, hardness (scratches glass), and association with manganese deposits. It is commonly found in Russia (Ural Mountains), Sweden, USA (Massachusetts, New Jersey), Australia, Brazil, Canada, Mexico, Japan, South Africa, and India. When evaluating rhodonite, look for good color saturation and interesting patterns of black manganese inclusions. For beads, consistency in size and hole quality is important. Be aware that some bright pink specimens may be dyed.