Not a diamond; appears to be raw crystalline mineral matrix, possibly calcite or quartz crystal formation in rock.
Not a diamond; appears to be raw crystalline mineral matrix, possibly calcite or quartz crystal formation in rock. · Raw crystal formation, uncut and unpolished.
Not applicable (Raw mineral specimen). Cut

Carat
Cannot be accurately determined as a single faceted stone; large specimen weight.
Color
Yellowish-white to opaque crystal matrix.
Clarity
Included / Heavily included with natural matrix.
Shape
Raw crystal formation, uncut and unpolished.
Overall Assessment
This specimen is a raw mineral formation rather than a cut diamond, displaying natural crystal faces and matrix.
Cut Quality
Not applicable (Raw mineral specimen).
Brilliance
Low to moderate vitreous luster typical of rough minerals.
Fire
Minimal to none due to lack of facet dispersion.
Scintillation
Poor due to raw, unfaceted surface.
Proportions
Natural formation proportions.
Symmetry
Natural crystal growth symmetry.
Polish
Unpolished natural crystal faces.
Fluorescence
Unknown without UV testing.
Inclusions
Abundant natural mineral inclusions and internal fractures.
Blemishes
Natural surface etching and rough texture.
Origin
Natural geological mineral deposit.
Treatment Detection
No treatments observed; appears completely natural.
Estimated Value
Varies by mineral type and specimen size as a mineral collector piece, typically low to moderate.
Certification Estimate
Mineralogical certification (e.g., GIA Gemological identification report) rather than diamond grading.
Investment Potential
Collected as a mineral specimen rather than an investment-grade gemstone.
Similar Diamonds
None (this is not a diamond).
Setting Suggestions
Display as a raw mineral specimen rather than jewelry setting.
Care & Maintenance
Dust gently with a soft brush; avoid harsh chemicals or ultrasonic cleaners depending on the specific mineral hardness.
Interesting Facts
Raw crystal clusters showcase natural geological growth patterns before human cutting and polishing.