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Olivine crystal orthorhombic Illustration and Icon
Olivine crystal orthorhombic
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Schematic depiction of an orthorhombic prismatic crystal characteristic of the olivine group. The image represents a mineral crystal (nesosilicate) within a rock-forming silicate hierarchy studied in mineralogy, crystallography, and petrology. Olivine occurs primarily in Earth’s upper mantle and in mafic to ultramafic igneous rocks, where it records Mg–Fe composition and magmatic conditions. The group spans the forsterite–fayalite solid solution, denoted Fo (forsterite, Mg2SiO4) and Fa (fayalite, Fe2SiO4). Functionally, this phase influences mantle rheology and serves as a geothermobarometric indicator.
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