Magnesio-riebeckite
A variety of Minerals
What is Magnesio-riebeckite?
Riebeckite is a sodium-rich member of the amphibole group of silicate minerals, chemical formula Na2(Fe3Fe2)Si8O22(OH)2. It forms a solid solution series with magnesioriebeckite. It crystallizes in the monoclinic system, usually as long prismatic crystals showing a diamond-shaped cross section, but also in fibrous, bladed, acicular, columnar, and radiating forms. Its Mohs hardness is 5.0–6.0, and its specific gravity is 3.0–3.4. Cleavage is perfect, two directions in the shape of a diamond; fracture is uneven, splintery. It is often translucent to nearly opaque.
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Key Characteristics
Formation of Magnesio-riebeckite
It typically forms dark-blue elongated to fibrous crystals in highly alkali granites, syenites, rarely in felsic volcanics, granite pegmatites and schist. It occurs in banded iron formations as the asbestiform variety crocidolite (blue asbestos). It occurs in association with aegirine, nepheline, albite, arfvedsonite in igneous rocks; with tremolite, ferro-actinolite in metamorphic rocks; and with grunerite, magnetite, hematite, stilpnomelane, ankerite, siderite, calcite, chalcedonic quartz in iron formations.
Quick Facts
Physical Properties
- Color
- Light blue to blue-black.
- Hardness (Mohs)
- 5 - 5.5
- Streak
- Pale grey to bluish-grey.
Chemical Properties
- Chemical Formula
- ◻{Na2}{Mg3Fe3+2}(Si8O22)(OH)2 Magnesio-riebeckite is defined as a member of the riebeckite group with Mg>Fe2+ in the C2+ position and (OH) in the W position.
- Elements
- Fe, H, Mg, Na, O, Si
Also Known As

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