Quartz is a silicon dioxide mineral known for its clarity and geometric crystal structure, often appearing clear to slightly cloudy depending on internal inclusions.
It forms through slow crystallization in hydrothermal environments and is used in electronics and timekeeping due to its piezoelectric properties.
This Specimen
This specimen features a semi-translucent body with noticeable internal clouding, creating a softer, less sharply defined appearance than clear quartz.
The crystal structure appears irregular, with variation in size and orientation rather than a uniform cluster of clean points.
The combination of internal haze and uneven formation gives the piece a more natural, less refined look compared to higher-clarity, sharply structured quartz.
Quartz is a silicon dioxide mineral known for its clarity and geometric crystal structure, often appearing clear to slightly cloudy depending on internal inclusions.
It forms through slow crystallization in hydrothermal environments and is used in electronics and timekeeping due to its piezoelectric properties.
This Specimen
This specimen features a semi-translucent body with noticeable internal clouding, creating a softer, less sharply defined appearance than clear quartz.
The crystal structure appears irregular, with variation in size and orientation rather than a uniform cluster of clean points.
The combination of internal haze and uneven formation gives the piece a more natural, less refined look compared to higher-clarity, sharply structured quartz.
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