Location | Arizona, United States |
Commodities Primary | Copper |
Commodities Secondary | Molybdenum,Lead, Silver, Gold, Zinc, Uranium |
Total Current Year Production | Period Ended December 31, 2022 |
Copper; pounds | 1,840,600,000 |
Molbdenum; pounds | 30,000,000 |
Lead; pounds | 0 |
Silver; ounces | 250,600 |
Gold; ounces | 31,100 |
Zinc; pounds | 0 |
Uranium; pounds | 0 |
Total Known Current and Historical Production | 1860 – 2021 |
Copper; pounds | 149,600,990,867 |
Molbdenum; pounds |
1,769,942,000 |
Lead; pounds |
2,212,268,238 |
Silver; ounces |
637,801,960 |
Gold; ounces |
16,631,450 |
Zinc; pounds |
2,212,268,238 |
Uranium; pounds |
0 |
Total Known Compliant Reserves | Proven & Probable |
Copper; pounds | 67,706,182,300 |
Molbdenum; pounds | 2,832,777,024 |
Lead; pounds | 0 |
Silver; ounces | 286,100,000 |
Gold; ounces |
0 |
Zinc; pounds |
0 |
Uranium; pounds |
0 |
Total Known Compliant Exclusive Resources | Measured & Indicated |
Copper; pounds | 144,450,354,652 |
Molbdenum; pounds | 3,675,976,162 |
Lead; pounds | 180,000,000 |
Silver; ounces | 313,300,000 |
Gold; ounces | 2,324,000 |
Zinc; pounds | 0 |
Uranium; pounds | 2,402,000 |
Inferred | |
Copper; pounds | 110,234,652,204 |
Molbdenum; pounds | 1,905,446,960 |
Lead; pounds | 44,000,000 |
Silver; ounces | 120,547,000 |
Gold; ounces |
295,500 |
Zinc; pounds |
0 |
Uranium; pounds | 277,782,120 |
Total Known Endowment | 1860 – 2021 |
Copper; pounds | 471,992,180,023 |
Molbdenum; pounds |
10,184,142,146 |
Lead; pounds |
2,436,268,238 |
Silver; ounces |
1,357,748,960 |
Gold; ounces |
19,250,950 |
Zinc; pounds |
2,212,268,238 |
Uranium; pounds |
280,184,120 |
Total Known Endowment includes current and historical production and compliant reserves and resources
Data compiled from DigiGeoData database, technical reports and corporate websites
DigiGeoData has compiled this information using best practices and does not warranty the completeness or accuracy.
All data should be checked and verified before use
The earliest miners in what is now Arizona were Native Americans who chiefly mined surface outcrops of salt, clays, hematite, quartz, obsidian, stone, turquoise, and coal.
In the late 1600s, Spanish explorers hunted for metallic deposits with especial interest in gold and silver.
Antonio de Espejo made the first major silver discovery south of the San Francisco Peaks in May 1583, near what some believe is present-day Jerome, Arizona.
By the late 17th Century, Spanish prospectors had engaged in extensive mining in the mountains bordering the Santa Cruz River and its tributary Sonoita Creek. Rare discoveries of sheets or “planchas” of silver – one sheet reportedly weighted 2700 pounds – fired the imaginations of several generations of miners. (Image to left: Early day miners stand in front of a mine portal near Morenci, AZ)
In 1854, in Ajo, Arizona, the Arizona Mining and Trading Company launched the modern era of hard-rock mining.
A burgeoning mining industry stimulated early growth in the Arizona Territory, and by 1864 nearly 25 percent of the male, non-native populace was prospectors.
By the 1870’s a plethora of hardrock mines were yielding prodigious volumes of copper, lead, zinc, silver and gold ore. In 1912, the newly christened state of Arizona supported 445 active mines, 72 concentrating facilities, and 11 smelters with a gross value of nearly 67 million dollars — equivalent to1.4 billion dollars in 2006 dollars.
Adapted from:
Arizona Geological Society
Arizona Historical Society
The geology of Arizona began to form in the Precambrian.
Igneous and metamorphic crystalline basement rock may have been much older, but was overwritten during the Yavapai and Mazatzal orogenies in the Proterozoic.
The Grenville orogeny to the east caused Arizona to fill with sediments, shedding into a shallow sea. Limestone formed in the sea was metamorphosed by mafic intrusions.
The Great Unconformity is a famous gap in the stratigraphic record, as Arizona experienced 900 million years of terrestrial conditions, except in isolated basins.
The region oscillated between terrestrial and shallow ocean conditions during the Paleozoic as multi-cellular life became common and three major orogenies to the east shed sediments before North America became part of the supercontinent Pangaea.
The breakup of Pangaea was accompanied by the subduction of the Farallon Plate, which drove volcanism during the Nevadan orogeny and the Sevier orogeny in the Mesozoic, which covered much of Arizona in volcanic debris and sediments.
The Mid-Tertiary ignimbrite flare-up created smaller mountain ranges with extensive ash and lava in the Cenozoic, followed by the sinking of the Farallon slab in the mantle throughout the past 14 million years, which has created the Basin and Range Province.
Arizona has extensive mineralization in veins, due to hydrothermal fluids and is notable for copper-gold porphyry, lead, zinc, rare minerals formed from copper enrichment and evaporites among other resources.
Adapted from Wikipedia
Coming Soon!
Coming Soon!
Copyright © 2021 DigiGeoData | Powered by ViaMarket
Data compiled from DigiGeoData database.
DigiGeoData has compiled this information using best practices and does not warranty the completeness or accuracy.
All data should be checked and verified before use