
mineral
Quartz with Spessartine Garnet and Biotite
SiO2 (Quartz) with Mn3Al2(SiO4)3 (Spessartine)
AI-generated identification · may be incorrectHardness of 7 for quartz and 6.5 to 7.5 for spessartine on the Mohs scale. Color is white/translucent quartz matrix with vibrant orange-red spessartine garnet crystals and dark biotite inclusions. Luster is vitreous to resinous. Crystal structure is trigonal (quartz) and isometric (garnet).…
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Physical properties
Hardness of 7 for quartz and 6.5 to 7.5 for spessartine on the Mohs scale. Color is white/translucent quartz matrix with vibrant orange-red spessartine garnet crystals and dark biotite inclusions. Luster is vitreous to resinous. Crystal structure is trigonal (quartz) and isometric (garnet). No cleavage for quartz, indistinct cleavage for garnet.
Formation & geological history
Formed in pegmatites or metamorphic hydrothermal environments where silica-rich fluids and manganese-rich solutions crystallize under high temperature and pressure conditions, often dating from Precambrian to Cenozoic eras depending on the specific geological location.
Uses & applications
Used primarily as a mineral specimen for collectors, in lapidary arts, and occasionally for metaphysical purposes or educational displays.
Geological facts
Spessartine is the manganese-aluminum endmember of the garnet group. The name comes from the Spessart region in Germany, though fine specimens are found worldwide in pegmatite pockets.
Field identification & locations
Can be identified by the translucent to milky white quartz host rock contrasted sharply with bright orange-red garnet crystal grains and dark mica flakes. Found in pegmatite-rich regions globally, especially in areas with granitic intrusions.
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