
mineral
Smoky quartz crystal cluster
Quartz, silicon dioxide (SiO₂), likely iron- or radiation-colored smoky quartz
AI-generated identification · may be incorrectHardness 7 Mohs; translucent brown to gray with vitreous luster, hexagonal crystal structure, and poor cleavage (conchoidal fracture). The specimen appears partly coated or included with darker matrix material.
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Physical properties
Hardness 7 Mohs; translucent brown to gray with vitreous luster, hexagonal crystal structure, and poor cleavage (conchoidal fracture). The specimen appears partly coated or included with darker matrix material.
Formation & geological history
Formed when silica-rich hydrothermal fluids or late-stage magma crystallized in cavities and fractures, commonly in granite or pegmatite. Its exact geological age cannot be determined from the photograph.
Uses & applications
Used as a collector specimen and occasionally in jewelry; quartz is also important in glassmaking, electronics, abrasives, and engineered stone.
Geological facts
Smoky coloration commonly results from irradiation affecting aluminum impurities in quartz. Crystal faces and conchoidal fractures help distinguish it from brown glass or calcite.
Field identification & locations
Identify by its glassy luster, hardness, six-sided crystal habit, and inability to scratch it with a steel knife; common sources include Brazil, the United States, Switzerland, and Madagascar.
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Sandstone (with potential mineral staining/concretions)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
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Granite
Granite (Phaneritic intrusive igneous rock)
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Septarian Pebble
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