Capgaronnite
A variety of Minerals

What is Capgaronnite?
Capgaronnite (HgS•Ag(Cl,Br,I)) is a mineral that forms small tufted aggregates or isolated crystals with a maximum width of 0.02mm and a maximum length of 0.1mm. This mineral is related to perroudite in chemical composition and crystal structure. Capgaronnite is associated with secondary minerals of Cu like olivenite, cyanotrichite, and tennantite.
Market Value Factors
Pricing varies for every rock and mineral, so use these universal factors to gauge Capgaronnite before comparing listings or appraisals.
Size & Weight
Larger, intact specimens usually command higher prices.
Rarity & Demand
Scarce material or popular varieties sell at a premium.
Condition & Finish
Chips, repairs, and heavy wear lower value; clean prep helps.
Treatment & Provenance
Untreated specimens with documented locality are prized.
Capgaronnite Localities Map
See where Capgaronnite is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.
Key Characteristics
Formation of Capgaronnite
Capgaronnite is a rare mineral that was observed in the Cap-Garonne copper-lead mine of Var, France. Capgaronnite is found in cavities of Triassic Conglomerate (geology) and Sandstone.
Quick Facts
Physical Properties
- Color
- Black, gray, greenish, yellow
- Density
- 6.19 g/cm³
- Streak
- Gray-black
Chemical Properties
- Chemical Formula
- AgHgClS Cl may be replaced by minor Br and I.
- Elements
- Ag, Cl, Hg, S

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Capgaronnite FAQs
How do I identify Capgaronnite?
Capgaronnite can be identified by its Black color. Look for these key characteristics when examining specimens.
What color is Capgaronnite?
Capgaronnite typically appears in Black, gray, greenish, yellow. Color can vary depending on impurities and formation conditions.
What is the formation of capgaronnite of Capgaronnite?
Capgaronnite is a rare mineral that was observed in the Cap-Garonne copper-lead mine of Var, France. Capgaronnite is found in cavities of Triassic Conglomerate (geology) and Sandstone.


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