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 features a rough, off-clear to milky tone with visible internal variation, giving it a more muted, less transparent appearance.
The surface is uneven and raw, with broken or irregular crystal faces rather than clean, sharply defined points.
The combination of lower clarity and rough texture gives the piece a more natural, unrefined look compared to smoother or more structured quartz.
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 features a rough, off-clear to milky tone with visible internal variation, giving it a more muted, less transparent appearance.
The surface is uneven and raw, with broken or irregular crystal faces rather than clean, sharply defined points.
The combination of lower clarity and rough texture gives the piece a more natural, unrefined look compared to smoother or more structured quartz.
