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Gold Bullion Mine (Copper Bullion Mine), Cherry, Cherry Creek District, Black Hills (Black Hill Range), Yavapai Co., Arizona, USA

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Latitude & Longitude (WGS84): 34° 35' 58'' North , 112° 3' 23'' West
Latitude & Longitude (decimal): 34.59945,-112.05639


‡Ref.: Wilson, E.D., Cunningham, J.B., and Butler, G.M. (1934), Arizona Lode Gold Mines and Gold Mining (revised 1967), Arizona Bureau of Mines Bull. 137: 31.

Anderson, C.A. & S.C. Creasey (1958), Geology and ore deposits of the Jerome area, Yavapai County, Arizona, USGS PP 308: 175.

U.S. Bureau of Mines - Arizona Bureau of Geology and Mining Technology file data.

Arizona Department of Mineral Resources Gold Bullion Mine file.

USGS Cherry Quadrangle map.

MRDS database Dep. ID #10048056, MRDS ID #M800023; and, Dep. ID #10109849, MRDS ID #M800222; and, Dep. ID #10234571, MAS ID #0040250780.

A former underground Cu-Ag-Au mine located about 1 mile NW of Cherry. Discovered 1896. Produced 1930-1937.

Mineralization is veins that pinch & swell to a maximum of 7 feet wide and contain lenses of quartz. It strikes N.15E. and dips 45ºW. Ore control was faulting. Ore concentration was oxidation at near surface. No alteration was noted. An associated rock unit is the Cherry Quartz Diorite (informal name).

Workings include a 660 foot deep incline and several 100 foot shallower workings.

Mineral List


6 valid minerals.

Regional Geology

This geological map and associated information on rock units at or nearby to the coordinates given for this locality is based on relatively small scale geological maps provided by various national Geological Surveys. This does not necessarily represent the complete geology at this locality but it gives a background for the region in which it is found.

Click on geological units on the map for more information. Click here to view full-screen map on Macrostrat.org

Paleoproterozoic
1600 - 2500 Ma
Cherry Tonalite

Age: Proterozoic (1600 - 2500 Ma)

Description: Medium- to medium-coarse-grained hornblende-biotite diorite to granodiorite containing phenocrysts of hornblende (Anderson and Creasey, 1967). Includes tonalite of Cherry (DeWitt, 1989), and part of Cherry batholith (Anderson, 1989a). Newly named herein for exposures near Cherry. Type area is designated where main mass exposed from north of Cherry to far southeastern part of map area. Smaller bodies exposed along east side of Lonesome Valley. Prominent north-trending zone of high magnetic intensity along eastern Lonesome Valley probably marks western contact of Cherry Tonalite with metavolcanic rocks (Langenheim and others, 2002). Most mafic along western margin of main mass and in southern Lonesome Valley. Exposed in erosional highs beneath Tertiary basalt from Interstate 17 to southern margin of map area. Cuts Bishop Spring Granodiorite (unit Xbp) northwest of Rugged Mesa. Cuts Bland Tonalite (newly named, unit Xbl) east of Perry Mesa and south of map area, along Squaw Creek. Undeformed in most outcrops, but mildly to strongly flow foli­ated in places. Strongly deformed along Shylock fault and Shylock high-strain zone in southwestern Black Hills. Hosts gold-bearing quartz veins in Cherry district that are genetically related to the tonalite (Clements, 1991). Chemically is calc-alkalic, sodic to very sodic, and very Mg rich to Fe rich. Age of sample from near Cherry, from U-Pb zircon analyses, is 1,740 Ma (Anderson and others, 1971). K-Ar hornblende dates of 1,694 and 1,690 Ma obtained from samples near Cherry (Lanphere, 1968; Dalrymple and Lanphere, 1971). 40Ar/39Ar total fusion date of 1,709 Ma obtained from one hornblende (Dalrymple and Lanphere, 1971). K-Ar biotite dates of 1,689–1,693 Ma also obtained from same samples. Con­flicting age (cuts 1,720-Ma Bland Tonalite but has U-Pb zircon age of 1,740 Ma) may be due to more than one tonalite body within a composite pluton (Anderson, 1989a)

Reference: DeWitt, E., V. Langenheim, E. Force, R.K. Vance, P.A. Lindberg, R.L. Driscoll. Geologic map of the Prescott National Forest and the headwaters of the Verde River, Yavapai and Coconino Counties, Arizona. Scientific Investigations Map SIM-2996. [99]

Statherian
1600 - 1800 Ma
Early Proterozoic granitic rocks

Age: Statherian (1600 - 1800 Ma)

Description: Wide variety of granitic rocks, including granite, granodiorite, tonalite, quartz diorite, diorite, and gabbro. These rocks commonly are characterized by steep, northeast-striking foliation. (1600-1800 Ma)

Comments: ~ 1.6 - 1.8 Ga

Lithology: Major:{granite,granodiorite,tonalite}, Minor:{quartz diorite,diorite,gabbro}

Reference: Horton, J.D., C.A. San Juan, and D.B. Stoeser. The State Geologic Map Compilation (SGMC) geodatabase of the conterminous United States. doi: 10.3133/ds1052. U.S. Geological Survey Data Series 1052. [133]

Data and map coding provided by Macrostrat.org, used under Creative Commons Attribution 4.0 License



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