Chalcopyrite: Difference between revisions
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[[File: | [[File:EastWhealTowan-chalcopyrite.jpg|thumb|right|frame|Unusually well formed chalcopyrite from East Wheal Towan, Porthtowan]] | ||
[[File:Ewtowan-chalcopyrite.png|right|frame|A curve trace of chalcopyrite from East Wheal Towan]] | [[File:Ewtowan-chalcopyrite.png|right|frame|A curve trace of chalcopyrite from East Wheal Towan]] | ||
Latest revision as of 07:14, 22 July 2026
- Lustre:Metallic
- Transparency:Opaque
- Colour:Brass yellow, often with an iridescent tarnish.
- Streak:Greenish black
- Hardness:3½ - 4 on Mohs scale
- Tenacity:Brittle
- Cleavage:Poor/Indistinct Indistinct on {011}, sometimes distinct.
- Fracture:Irregular/Uneven
Chalcopyrite is the main ore of copper, is softer than pyrite and fairly easy to find in usable quantities. It's rarely well crystallised, but forms thick veins and large blobs, usually in quartz.
Due to the copper content it has a very low overall resistance, I find it one of the easiest minerals to find good semiconducting junctions, it doesn't seem to alter much with oxidisation or weathering. Unlike pyrite it doesn't seem to vary much between sites or occurrences. As you can see in the curve trace, it's particularly susceptible to noise - during performances I tend to start with chalcopyrite or chalcocite as they are particularly 'eager' low resistance semiconductors compared to some galena or cassiterite.
Famously it was combined with zincite to build bi-crystal "Perikon" detectors, invented in 1908 by Greenleaf Whittier Pickard.