Quartz is a silicon dioxide mineral known for its clarity and geometric crystal structure, typically appearing clear to 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 more opaque body with a higher concentration of internal inclusions, giving it a denser, less transparent appearance.
The surface appears irregular and slightly rough, with uneven crystal development rather than clean, sharply defined points.
The combination of reduced clarity and uneven structure creates a more textured, grounded look compared to clearer, more refined quartz specimens.
Quartz is a silicon dioxide mineral known for its clarity and geometric crystal structure, typically appearing clear to 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 more opaque body with a higher concentration of internal inclusions, giving it a denser, less transparent appearance.
The surface appears irregular and slightly rough, with uneven crystal development rather than clean, sharply defined points.
The combination of reduced clarity and uneven structure creates a more textured, grounded look compared to clearer, more refined quartz specimens.
Image 1 of 5
Image 2 of 5
Image 3 of 5
Image 4 of 5
Image 5 of 5