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riebeckite : ウィキペディア英語版
riebeckite

Riebeckite is a sodium-rich member of the amphibole group of silicate minerals, chemical formula ☐Na2(Fe2+3Fe3+2)Si8O22(OH)2. It forms a 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.
==Name and discovery==
It was first described in 1888 for an occurrence on Socotra Island, Aden Governorate, Yemen and named for German explorer Emil Riebeck (1853–1885).〔

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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