| Lat / long: | 33.10732, -109.39065 |
| Primary: | Copper |
| Orebody form: | UNKNOWN |
| Operation type: | Unknown |
| Production size: | Small |
| Development status: | Producer |
| First production started: | 1915 |
| Host type: | Quartzite,Granite |
| Associated rock: | Coronado Quartzite;Precambrian Granite Basement |
| Associated type: | Diabase |
| Structure: | Ne Side Of Prominent Quartzitic Ridge North Of Morenci; Ridge Forms The Divide Between Eagle Creek And Chase Creek Watersheds; Block Faulting South Of The Great Coronado Fissure With Downthrow Of 1200 Ft On Southern Side, Minor W-E Trending Faults; Locality Is Cut By Occasional Dikes Of Diabase And Porphyry |
| Tectonic: | Precipitous Gully Terrain East Of Coronado Massif; Massif Surrounded By Peripheral Faults |
| Alteration processes: | Surface Oxidation To Unknown Depths |
| MRDS | M800421 |
| DEP | 10048291 |
| Reference | {Deposit:: ABGMT-USBM FILE DATA.}{Deposit:: BLM DISTRICT SHEET 840.}{Deposit:: ABGMT CLIPPINGS FILE, CORONADO COPPER CO, ARIZONA COPPER CO LTD.}{Deposit:: USGS PP 43, P. 338-346.}{Deposit:: BENNETT, K. C. 1975, GEOLOGY AND ORIGIN OF THE BRECCIAS IN THE MORENCI-METCALF DISTRICT, GREENLEE COUNTY, ARIZONA: M. S. THESIS, UNIVERSITY OF ARIZONA, 153 P.}{Other Database:: CIMRI} |
| Reporter | Calder, Susan R. |