Not a diamond; this is a raw mineral matrix showing crystalline quartz interspersed with iron oxide or hematite staining.
Not a diamond; this is a raw mineral matrix showing crystalline quartz interspersed with iron oxide or hematite staining. · Rough uncut matrix / irregular crystalline aggregate
Uncut / Raw mineral state Cut
Carat
Not applicable (raw mineral specimen)
Color
Colorless to white with prominent reddish-orange patches
Clarity
Included / Heavily flawed due to internal fractures and mineral inclusions
Shape
Rough uncut matrix / irregular crystalline aggregate
Overall Assessment
An interesting raw mineral specimen featuring translucent quartz growth and iron staining, entirely distinct from diamond.
Cut Quality
Uncut / Raw mineral state
Brilliance
Vitraneous to greasy luster on fractured surfaces, limited white light return
Fire
Minimal to none due to lack of faceted geometry
Scintillation
Poor due to lack of polished facets and optical symmetry
Proportions
Not applicable to raw crystalline aggregates
Symmetry
Natural asymmetrical formation
Polish
Unpolished natural fracture surface
Fluorescence
Indeterminate from visual inspection
Inclusions
Numerous internal micro-fractures, mineral grains, and particulate inclusions
Blemishes
Natural surface irregularities, pits, and weathering marks
Origin
Natural geological formation within a pegmatitic or hydrothermal vein system
Treatment Detection
No signs of enhancement or artificial treatment
Estimated Value
Nominal value as a raw mineral specimen
Certification Estimate
Gemological laboratories would issue a mineral identification report rather than a diamond grading report
Investment Potential
Collector value only, no traditional gemstone investment potential
Similar Diamonds
None (this is quartz, not diamond)
Setting Suggestions
Wire-wrapped or bezel setting if displayed as a raw mineral specimen
Care & Maintenance
Standard mineral specimen care; avoid harsh chemicals and abrasive impacts
Interesting Facts
Often mistaken for rough gem material by novices due to its crystalline structure