Obvious connection because nearly all the ores that produce metals are composed of minerals.
Take just one example: Copper
Link to the Los Alamos Periodic Table or the more detailed Web Elements Periodic Table
Amazing diversity of relatively important copper-bearing minerals and deposit types.
| Copper | Cu |
| Cuprite | Cu2O |
| Tenorite | CuO |
| Chalcocite | Cu2S |
| Digenite | Cu9S5 |
| Covelite |
CuS |
| Chalcopyrite | CuFeS2 |
| Bornite |
Cu5FeS4 |
| Azurite | Cu3(CO3)2(OH)2 |
| Malachite |
Cu2CO3(OH)2 |
| Atacamite | Cu2Cl(OH)3 |
| Antlerite | Cu3SO4(OH)4 |
| Brochantite |
Cu4SO4(OH)6 |
| Chrysocolla | Cu4H4Si4O10 (OH)8 |
| Dioptase |
Cu6Si6O18 6H2O |
| Enargite | Cu3AsS4 |
| Luzonite | Cu3AsS4 |
| Famatinite | Cu3SbS4 |
| Tennantite | Cu12As4S13 |
| Tetrahedrite |
Cu12Sb4S13 |
| Kostovite | CuAuTe4 |
| Stannite | Cu2FeSnS4 |
| Torbernite | Cu(UO2)2(PO4)2 8-12H2O |
| Turquoise |
CuAl6(PO4)4(OH)8 5H2O |
Look at some examples with direct (or indirect) connections to Wisconsin:
Native Copper District - history and decline
White Pine District - history and mineralogy - development of ideas on replacement of sulfides
Porphyry Copper Deposits - the next Big thing - understanding of hydrothermal alteration, exploration clues
Massive Sulfide Deposits - the name says it all - morphology depends on setting and density and temperature of the hydrothermal fluid.
An old estimate for the Crandon Deposit:
Tons of Ore % Cu % Pb % Zn g/t Ag g/t AuZinc - Massive Ore 42,900,000 0.6 0.73 8.40 52.6 1.4Cu - Stringer Ore 24,500,000 1.8 0.03 0.71 10.0 0.3Total 67,400,000 1.0 0.5 5.6 36.8 1.0Approximate Value/ton $96 $25 $4 $50 $7 $10
Weathering and Supergene Enrichment of Copper Ores - Frosting the Cake
Beginning of a Trip to the Flambeau Mine
Magmatic copper sulfide ores - Sudbury Ontario