Mineral
Forsterite
Silicate Minerals
Forsterite (Mg2SiO4, also known as white olivine) is the magnesium-rich end member of the olivine solid solution series and is isomorphous with the iron-rich end member, fayalite. It crystallizes in the orthorhombic system and is associated with igneous and metamorphic rocks, and it has been found in meteorites, in cometary dust returned by the Stardust probe in 2005, and as tiny crystals in the dusty gas clouds around a forming star. Peridot is the gemstone variety of forsterite olivine. In this atlas it is the mineral species that the gemstone peridot records.
Forsterite (Mg2SiO4, also known as white olivine) is the magnesium-rich end member of the olivine solid solution series and is isomorphous with the iron-rich end member, fayalite. It crystallizes in the orthorhombic system and is associated with igneous and metamorphic rocks, and it has been found in meteorites, in cometary dust returned by the Stardust probe in 2005, and as tiny crystals in the dusty gas clouds around a forming star. Peridot is the gemstone variety of forsterite olivine. In this atlas it is the mineral species that the gemstone peridot records.
Facts
Chemical Formula Chemical Formula Hardness (Mohs) Hardness (Mohs) Classification
Strunz Class Strunz Class Crystal System Crystal System Connections
Caused By
Source Forsterite (Wikipedia)
Source Forsterite (Wikipedia)
Source Forsterite (Wikipedia)
Crystallizes In System
In Discipline
In the Other Atlases
Mineral Species Of
Also in Divinity Atlas: of this mineral species.
Sources
1. Forsterite (Wikipedia)
Wikimedia FoundationForsterite, lead paragraph
is the magnesium-rich end-member of the olivine solid solution series
Forsterite, article text
Peridot is the gemstone variety of forsterite olivine.
View the Source 2. Webmineral: Forsterite
WebmineralColor field
Colorless, Green, Yellow, Yellow green, White.
Luster field
Vitreous (Glassy)
View the Source Forsterite (Wikipedia)
Caused By: Fractional Crystallization, Geologic occurrence
Due to its high melting point, olivine crystals are the first minerals to precipitate from a magmatic melt in a cumulate process, often with orthopyroxenes.
Caused By: Magmatism, Geologic occurrence
Forsterite-rich olivine is a common crystallization product of mantle-derived magma.
Caused By: Metamorphism, Geologic occurrence
Forsterite also occurs in dolomitic marble which results from the metamorphism of high magnesium limestones and dolomites.
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