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Key facts
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Search for specimens: View all chrysocolla specimens from Morenci Mine, Arizona, USA
Morenci Mine lies at Morenci in Greenlee County, Arizona, about 50 miles northeast of Safford on U.S. Highway 191. It is an active open-pit copper-molybdenum mining complex, historically known under names including Morenci pit, Phelps Dodge Morenci Mine, and Morenci-Metcalf. The deposit belongs to the Clifton-Morenci, or Copper Mountain, mining district near the Arizona-New Mexico border.
Geologically, Morenci is a large porphyry copper system with oxide, secondary sulfide, and primary sulfide mineralization. The district includes early Proterozoic schist and granite, Paleozoic and Cretaceous sedimentary sequences, and early to middle Tertiary intrusive and volcanic rocks. The copper system developed with intrusive activity, hydrothermal alteration, and later supergene oxidation and enrichment. Laramide porphyries intruded older sedimentary rocks and produced skarn assemblages in places, while the broader ore system records potassic, sericitic, propylitic, and argillic alteration. In the oxidized and acid-soluble oxide ore, chrysocolla occurs with malachite, azurite, brochantite, and locally minor chalcocite, pyrite, and cuprite.
The supergene story is central to Morenci chrysocolla. Multiple cycles of leaching and enrichment attacked primary sulfides and produced both a secondary sulfide blanket and copper oxide zones. Oxidation and enrichment were strongly controlled by faults, fractures, paleotopography, climate, and hydrology. Enrichment and oxidation zones tend to thicken in valleys and thin over ridges, and the long-lived enriched zone was localized in the ancestral Chase Creek Canyon. The Northwest Extension area, Western Copper area, Metcalf pit, Southside/Azurite pit area, and older mine areas all figure in the specimen and research literature.






Morenciâs mining history is as important as its geology. Copper mineralization in the district attracted attention in the 1860s, and early prospectors were drawn by the blue and green copper staining. In the nineteenth century, only very high-grade copper ore could pay because transportation costs were severe. Ore was hauled and trammed from mines high on the mountains down toward Clifton, where smelters had water from the San Francisco River. Phelps Dodge & Company entered the district in 1881 with a $50,000 investment and eventually consolidated operations by 1921. Underground mining gave way to open-pit mining beginning in 1937, and Morenci has been in continuous open-pit operation since 1939. The Morenci concentrator was commissioned in 1942, Metcalf began receiving ore in 1975, the first SX/EW plant was commissioned in 1987, and the last Morenci smelter closed in 1984.çŸä»£ã®ã¢ã¬ã³ã·ã¯ãã«ãžã¥ã¢ã«ãªæ¡éå°ã§ã¯ãããŸãããããªãŒããŒãã»ãã¯ã¢ã©ã³ãéå¶ããå€§èŠæš¡ã§æŽ»åçãªé±å±±ã§ãããããªãŒããŒãã72%ã®æªå岿åããäœåã°ã«ãŒãé¢é£äŒæ¥ãæ®ãã®28%ãä¿æããŠããŸããã¢ã¯ã»ã¹ã¯ç®¡çãããç£æ¥çã§å®å šèŠå¶ãé©çšãããŠãããäŸµå ¥ã¯æ³çã«ãå®å šçã«ãèªããããŠããŸãããæŽå²çã«éèŠãªæšæ¬ååã¯ãæ£åŒãªæ¡éå¥çŽãéããŠè¡ãããç¹ã«1974幎ã«å§ãŸã£ããã«ãã¹ã»ãodgeã®ãµãŠã¹ãŠã§ã¹ãéšéãšã®ã¹ãŠã§ã¹ãã»ããã©ã«ã»ã¢ãœã·ãšã€ãå¥çŽãéèŠã§ããããã®å¥çŽã«ãããã¡ãã«ãŒãããã³ã¢ã¬ã³ã·ã®ãã®ä»ã®å°åãããæµžåºæ³ã®ãã³ããžè¡ãããšã«ãªã£ãŠããæšæ¬ãä¿è·ãããŸããããã®ãããªå ¬èªäœæ¥ä»¥å€ã§ã¯ãæšæ¬ååã¯çšã§æ©äŒçãªãã®ã§ãããçŸåšã®é±å±±æ¹éã¯ã¢ã¬ã³ã·ãã¬ã¯ãªãšãŒã·ã§ãã«ãªæ¡éãµã€ãã«ã¯ããŠããŸããã
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Morenci chrysocolla should be evaluated first as a locality specimen and second as chrysocolla. The strongest pieces show a believable Morenci assemblage: chrysocolla with malachite, azurite, tenorite, quartz or chalcedony, iron oxides, and the distinctive dark oxide matrices common to the district. Old labels from Phelps Dodge Morenci Mine, Morenci-Metcalf, Northwest Extension, Metcalf pit, or a named collection can matter greatly, especially because Morenci azurite-malachite specimens have often been confused with Bisbee. In expert discussions of Morenci material, minor chrysocolla has even been cited as a useful clue for distinguishing certain Morenci specimens from Bisbee look-alikes.
There is no widely documented Morenci-specific chrysocolla fake tradition comparable to the well-known fakery problems in some other mineral categories. The practical risks are more ordinary but still important: dyed blue stone sold as chrysocolla, stabilized material not disclosed, polished lapidary material sold with vague or inflated locality claims, and chrysocolla-bearing pieces confused with turquoise or gem silica. Because raw chrysocolla can be soft, porous, and brittle, stabilization with resin is a real issue in the trade. Stabilization is not automatically disqualifying for a fragile matrix specimen if it is disclosed, but undisclosed resin affects value and should be treated as a condition issue.
Condition is the chief challenge. Morenci chrysocolla can crack, powder, bruise, or detach from matrix, particularly when it occurs as thin blue layers or chalky botryoidal skins. Edges of old pocket plates are often contacted where they were removed from the pocket wall, and malachite or azurite crystals on chrysocolla may show small nicks. Avoid aggressive cleaning. Acids, prolonged soaking, ultrasonic cleaning, and hard brushing can damage soft chrysocolla, loosen botryoids, or dull associated malachite and azurite. Store away from abrasion, heat, and direct harsh sunlight, and handle specimens by the matrix rather than by the blue surface.
Availability is moderate but uneven. Morenci is a famous and long-lived copper mine, so chrysocolla-bearing specimens appear regularly in dealer inventories and auctions, especially as chrysocolla with malachite, chrysocolla with azurite, or chrysocolla-rich oxide matrix. However, fine undamaged locality pieces with strong aesthetics and old provenance are not abundant. Northwest Extension azurite-malachite specimens, 5000-foot-level chrysocolla-malachite pieces, and older Southwest Mineral Associates material are more collectible than generic âMorenci chrysocollaâ chunks. Prices can range from accessible small specimens to serious cabinet-level pieces, with value rising sharply for documented history, vivid color, undamaged botryoidal surfaces, azurite or malachite contrast, and gem silica character.## Story & Field Notes
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ãã®ã¯ãªã¹ãã¹ã€ãã®è©±ã¯ãã«ããŒè²ã§ã¯ãªãèé é±ã®è©±ãšããŠã¯çãããã¢ã¬ã³ã·ã®æšæ¬ãããã«äŸ¡å€ãããããæ£ç¢ºã«ãšãããŠãããæ¥ã æ°åäžãã³ãšããéã®é±ç³ãæ¬åºããé±å±±ã§ã¯ãèµ€ãæ³¥ã®äžã®ã²ãšç®ã«éãæ ããã±ãããçŸããæ°åã®èªå®æ¡æè ã«ãã£ãŠäœæéãæããããã®åŸäžå€ã§çç£ã®è«çãžãšæ¶ããŠããŸãããšããããã¢ã¬ã³ã·ã®ã¯ããµã€ãã¯ãåãäžçã«å±ãããã®ã§ããïŒçŸãããå°è³ªçã«ç€ºåã«å¯ã¿ã誰ããæéå ã«ãããèªèããªãéããé ã®äŸçµŠãžãšåãããªã¹ã¯ãåžžã«æ±ããŠããã## é±ç©åŠçèšé²ãšåºçç©- Mindat occurrence record: Chrysocolla from Morenci Mine, Morenci, Greenlee County, Arizona, USA â Morenciã§ã®ãã§ãŒã¯ç³ã®çºçèšé²ãåŒãçç©åŠçé¢é£é±ç©ã®åçããŒã¿ãåç §å²ãèšé²ããŸãã
Mindat locality page: Morenci Mine, Morenci, Greenlee County, Arizona, USA â 座æšãå¥åãé±ç©ãªã¹ããæ¡é±ã»å°è³ªããŒããé¢é£ãµãããŒã«ãªãã£ãå«ãã³ã¢å±å°èšé²ã
Lindgren, W. (1905). âThe copper deposits of the Clifton-Morenci district, Arizona.â U.S. Geological Survey Professional Paper 43, 375 p. â å°åºã®å°è³ªãšé é±åºã«é¢ããç±³åœå°è³ªèª¿æ»æã®åºç€çã¢ãã°ã©ãã
Enders, M. S. (2000). âThe Evolution of Supergene Enrichment in the Morenci Porphyry Copper Deposit, Greenlee County, Arizona.â PhD dissertation, University of Arizona. â Morenciã®è¡šé¢é žåéçšãé žåé±ç©åããã§ã¯ã»ã³ã¯é±ç©ãå«ã詳现ãªåå£«è«æã
Melchiorre, E. B., and Enders, M. S. (2003). âStable Isotope Geochemistry of Copper Carbonates at the Northwest Extension Deposit, Morenci District, Arizona: Implications for Conditions of Supergene Oxidation and Related Mineralization.â Economic Geology 98(3), 607â621. â Northwest Extensionã®azuriteãš malachiteã®åäœäœç ç©¶ãMorenciã®é žåç°å¢ã®çé žå¡©åŽã®çè§£ã«éèŠã
Schumer, B. N., Stegen, R. J., Barton, M. D., Hiskey, J. B., and Downs, R. T. (2019). âMineralogical Profile of Supergene Sulfide Ore in the Western Copper Area, Morenci Mine, Arizona.â The Canadian Mineralogist 57(3), 391â401. â Western Copperå°åã®è¶ çå°ç¡«åé±ç©ã®çµæ¶åŠçç¹æ§ãšçµæã®æè¡çç ç©¶ã
Hay, M., and Wilson, W. E. (2020). âThe Morenci District, Greenlee County, Arizona.â The Mineralogical Record 51, 71â118. â Morenciã®æŽå²ãšé±ç©æšæ¬ãç¹éãããã³ã¬ã¯ã¿ãŒåãã®äž»èŠãªå°åºèšäºã
Presmyk, L. (2023). âThe Mines and Minerals of the Copper Mountain Mining District, Morenci, Greenlee County, Arizona, USA.â New Mexico Mineral Symposium abstract. â åææšæ¬ã誀ã©ãã«ä»ããSouthwest Mineral AssociatesãèåãªMorenciã®çºèŠã«é¢ããèŠç¹ããŸãšããã³ã¬ã¯ã¿ãŒåãæŽå²ã
Freeport-McMoRan Technical Report Summary for Morenci Mine, Arizona, U.S., as of December 31, 2025 â çŸåšã® deposit typeã ownershipã reservesã processingã ããã³çŸä»£çãªå°è³ªè§£éã®æè¡çåºå žã
Mindat photo record 470081: Chrysocolla with Tenorite, Morenci Mine â æãããªèè²ã®ã¯ãªãœã³ã©çã2.5 à 1.5 à 1ã€ã³ãã®æšæ¬äžã«ããå ¬éèšé²ã
Mindat photo record 621829: Chrysocolla pseudomorphs after Azurite, Morenci Mine â ã¢ãºã©ã€ãã®åœååŸã®ã¯ãªãœã³ã©ã12 mmã®èŠéã§ç€ºãææžã
Mindat photo record 633711: Gemmy chrysocolla / gem silica, Morenci Mine â éå æ§ã®èç¶ç©ãå«ã倧ã㪠gemmy ã¯ãªãœã³ã©æšæ¬ãšãèãæè²ã®ã¯ãªãœã³ã©ã®çžãææžåã
Mindat photo record 299858: Chrysocolla with Malachite, Morenci Mine, 5000 ft. Level â ç²æ«ç¶ã®éãã¯ãªãœã³ã©ãããªãªã€ããšãžã§ã æã®ãããã©ã«ã€ãããŒãŒãããããã³éåžžã«å ·äœçãªéå±€æ å ±ãææžåã
Wikimedia Commons: Malachite-Chrysocolla-181378.jpg â Harold Urish ã³ã¬ã¯ã·ã§ã³ç±æ¥ã® Morenci ãã©ã«ã€ã-ã¯ãªãœã³ã©æšæ¬ïŒ9.3 à 7.8 à 5.7 cmïŒã®ãèªç±ã©ã€ã»ã³ã¹åçã## Videos & Media
âMorenci: Deep Roots, Broad Horizonsâ â Freeport-McMoRan â Freeport-McMoRanã®åç±³äºæ¥ããŒãžã«åã蟌ãŸãã21:46ã®äŒæ¥åç»ãçŸåšã® Morenci ææ¥ã®èŠæš¡ãšå°å瀟äŒã®ç¶æ³ãçè§£ããã®ã«åœ¹ç«ã¡ãŸãã
âArizona Copper Miningâ â Freeport-McMoRan â Freeportã®åç±³äºæ¥ã¡ãã£ã¢ã«åã蟌ãŸããã¢ãªãŸãå·ã®é 鱿¥ã®æŠèŠåç»ïŒ2:11ïŒã
âMolybdenum Operationsâ â Freeport-McMoRan â Morenciã®é -ã¢ãªããã³çç£ã®æèã«é¢é£ãã2:11ã®åç»ã
Mine Rat Minerals: âThe Incredible âPigment Zoneâ of Azurite, Morenci, Arizonaâ â Mark Kielbasoã«ããã1992幎㮠Northwest Extension ã¢ãºã©ã€ãçºèŠã®åçãæ·»ããéå€ã¹ããŒãªãŒã## ãããªãèªæžãšå€éšãªã³ã¯
Mindat: Morencié±å±±ããã®ã¯ã«ã»ã³ãŒã© â ã¯ã«ã»ã³ãŒã©ã®ç£åºããŒã¿ãé¢é£æ§ãåçããŒã¹ã®ç£å°èšé²ã®æé©ãªåºçºç¹ã
Mindat: Morencié±å±±ã®ç£å°ããŒãž â åºç¯ãªé±ç©ãªã¹ããç£å°ããŒã¿ãå¥åã座æšãæŽå²çã»å°è³ªåŠçããŒãã
Mindat: Morencié±å±±ãã©ãã®ã£ã©ãªãŒ â å®ç© Morenciæšæ¬ã®ç¿æ§ããããªã¯ã¹ãé±ç©çµæ¶ã®æ¯èŒã«æçšã
Freeport-McMoRan: åç±³ã®ææ¥ â Morenci â Morenciã®æææš©ãæœèšãé±ç³çš®ãææ¥èŠæš¡ã®å ¬åŒçŸæ³ãœãŒã¹ã
Freeport-McMoRan Morenci æè¡å ±åãµããªãŒã2025å¹Žæ«æç¹ â çŸåšã®å°è³ªãåèµéãåŠçãé±å±±ã®æèã詳述ããæè¡å ±åã
USGS Professional Paper 43: ã¢ãªãŸãå·ã¯ãªããã³-ã¢ã¬ã³ã·å°åºã®é é±åº â ã¯ã«ãããŒã»ãªã³ãã¬ã³ã«ãã1905幎ã®å€å žçå°åºã¢ãã°ã©ãã
ãã¥ãŒã¡ãã·ã³é±ç©ã·ã³ããžãŠã èŠæš: é å±±é±åºã®é±å±±ãšé±ç© â Les Presmykã«ããåªããèŠçŽçã³ã¬ã¯ã¿ãŒå²ããŒã¿ã
The Mineralogical Record ãµã³ãã«å·: Morenciå°åºãã°ãªãŒã³ãªãŒé¡ãã¢ãªãŸã â Mark HayãšWendell E. Wilsonã«ããã³ã¬ã¯ã¿ãŒäžå¿ã®èšäºã
Mine Rat Minerals: é©ãã¹ããçè²ãŸãŒã³ãAzuriteãMorenciãã¢ãªãŸã â 1992幎 Northwest Extension çºèŠæã®äžäººç§°æ¡éèšã
MineralAuctions: Northwest Extension Morenciã®äºäŸ â Morenci Northwest Extensionã®ã¢ãºã©ã€ã-ãã©ã«ã€ã cabinetææãšæè¿ã®ãªãŒã¯ã·ã§ã³å±¥æŽã®æçšãªåžå Žåç §ã
Minfind: Morencié±å±±ã®ã¯ã©ãŒãä»ãã¯ã«ã»ã³ãŒã©ãšãã©ã«ã€ãïŒPhelps Dodge Morenci MineïŒ â 1960幎代åé ã® Morenci ã¯ã«ã»ã³ãŒã©-ãã©ã«ã€ã-ã¯ã©ãŒãæšæ¬ãšé瀺ãããå®å®åã®èšé²ã
Wikimedia Commons: Malachite-Chrysocolla-181378.jpg â Morenciã®ãã©ã«ã€ã-ã¯ã«ã»ã³ãŒã©æšæ¬ã®ãªãŒãã³ã©ã€ã»ã³ã¹ç»åãšããŒã¿ã