
mineral
Seraphinite
Clinochlore (Mg,Fe2+)5Al(Si3Al)O10(OH)8
AI-generated identification · may be incorrectHardness: 2-4 on Mohs scale; Color: dark green to gray with silver chatoyant inclusions; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect mica-like cleavage; Specific gravity: 2.55-2.75
- Hardness
- 2-4 on Mohs scale
- Color
- dark green to gray with silver chatoyant inclusions
- Luster
- Vitreous to pearly
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Physical properties
Hardness: 2-4 on Mohs scale; Color: dark green to gray with silver chatoyant inclusions; Luster: Vitreous to pearly; Crystal structure: Monoclinic; Cleavage: Perfect mica-like cleavage; Specific gravity: 2.55-2.75
Formation & geological history
Formed as an alteration product of magnesium-rich minerals like pyroxene, biotite, and amphibole. It is a specific gem-grade variety of clinochlore formed in metamorphic environments, primarily in the Pre-Cambrian Korsthunovskoye deposit.
Uses & applications
Primarily used as a decorative stone, in jewelry (cabochons, pendants), and for metaphysical or collection purposes. It is too soft for rings but popular for earrings and necklaces.
Geological facts
Its name is derived from the 'Seraphim' (the highest order of angels) because the feathery silver mica inclusions resemble wings. It is almost exclusively found in the Lake Baikal region of Siberia.
Field identification & locations
Identify by its unique 'feathery' silver chatoyancy (shimmer) against a forest green background. It is relatively soft and can be scratched with a copper coin. Look for the distinct radial patterns of chlorite fibers.
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Sandstone (with potential mineral staining/concretions)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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