Hillside Mine, Bozarth Mesa, Bagdad, Eureka Mining District, Yavapai County, Arizona, USAi
| Regional Level Types | |
|---|---|
| Hillside Mine | Mine |
| Bozarth Mesa | Mesa |
| Bagdad | Census-designated Place |
| Eureka Mining District | Mining District |
| Yavapai County | County |
| Arizona | State |
| USA | Country |
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Latitude & Longitude (WGS84):
34° 37' 58'' North , 113° 12' 34'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
| Place | Population | Distance |
|---|---|---|
| Bagdad | 1,876 (2016) | 5.8km |
| Wikieup | 133 (2011) | 37.5km |
| Peeples Valley | 428 (2011) | 59.9km |
| Congress | 1,975 (2014) | 61.8km |
| Yarnell | 649 (2011) | 62.3km |
Other/historical names associated with this locality:
Happy Jack MS 920 claim; Camp MS 919 claim; Seven Stars MS 916 claim
A former underground Au-Ag-Zn-Pb-Cu-U-V mine located on 6 patented claims in sec. 16 & 21, T.15N., R.9W., Boulder Creek vicinity, a little more than 3 miles north of Bagdad and east of Bozarth Mesa. located March 11, 1887 by John Lawler and B.T. Riggs. Discovered on March 11, 1887 and owned by John Lawler & B.T. Riggs, then sold to H.H. Warner (June, 1890-1904)(Seven Stars Mining Co.); John Lawler (1904- ); Hillside Mines, Inc. (1934-1940); Boulder Mining Co. (1940-1942); State of Arizona (1942-1944); East Vulture Mining Co. (1944-1951).
The deposit is a typical fissure vein in muscovite schist, an important member of the Yavapai schist. The vein has a N.10ºW. strike at the south end and changes to a N.25ºE. strike at the north end. The dip is not uniform but averages between 75º to 80º in a westerly direction. Faulting before and after mineralization has been important. The main vein and several branches occupy a zone of faults antedating the veins, and sufficient movement along the faults occurred after mineralization to form a 3 foot zone of gouge and fault breccia in which unbrecciated vein material is found as irregular veinlets. Branching veins appear on both sides of the main vein and those to the east in general dip west less steeply than the main vein, whereas those on the west side of the main vein are nearly vertical. Small veinlets of sulfide, with or without quartz, fill minor fractures in the Hillside Mica Schist. The main vein averages 2½ feet (75 cm) in width on the upper levels and 4 feet on the 800 & 900 levels.
Four periods of quartz-sulphide deposition have been recognized from the banding and local comb structure. Some intramineralization faulting is indicated by microbrecciation of the sulphides and cementation by later quartz. The common sulphide minerals occur usually in blebs or bunches in quartz.
Strike faults locally cut out the vein and elsewhere repeat it. In other places the vein has been broken so completely as to form only an unrecognizable part of the gouge. After the strike faulting that followed mineralization there were offsets along north-dipping (25º-45º) cross faults. In general these late cross faults have formed clean-cut breaks, and the vein on the hanging wall side of the cross faults has been displaced 1 to 25 feet eastward.
Workings include 7,000 of development work by Lawler (1887-1892), by 1914 there were some 11,000 feet of workings, ultimately over 16,000 feet of workings. The shaft is 765 feet deep to the 1000 level. The vein was worked for 2,400 feet along the strike and stoped almost completely above the 700 level for an average length of 2,000 feet. Production included 58,748 oz. Au, 1,315,264 oz. Ag, 6,503,028 pounds Pb, 3,300,524 pounds Zn and 398,813 pounds of Cu. (to 1951).
The deposit is a typical fissure vein in muscovite schist, an important member of the Yavapai schist. The vein has a N.10ºW. strike at the south end and changes to a N.25ºE. strike at the north end. The dip is not uniform but averages between 75º to 80º in a westerly direction. Faulting before and after mineralization has been important. The main vein and several branches occupy a zone of faults antedating the veins, and sufficient movement along the faults occurred after mineralization to form a 3 foot zone of gouge and fault breccia in which unbrecciated vein material is found as irregular veinlets. Branching veins appear on both sides of the main vein and those to the east in general dip west less steeply than the main vein, whereas those on the west side of the main vein are nearly vertical. Small veinlets of sulfide, with or without quartz, fill minor fractures in the Hillside Mica Schist. The main vein averages 2½ feet (75 cm) in width on the upper levels and 4 feet on the 800 & 900 levels.
Four periods of quartz-sulphide deposition have been recognized from the banding and local comb structure. Some intramineralization faulting is indicated by microbrecciation of the sulphides and cementation by later quartz. The common sulphide minerals occur usually in blebs or bunches in quartz.
Strike faults locally cut out the vein and elsewhere repeat it. In other places the vein has been broken so completely as to form only an unrecognizable part of the gouge. After the strike faulting that followed mineralization there were offsets along north-dipping (25º-45º) cross faults. In general these late cross faults have formed clean-cut breaks, and the vein on the hanging wall side of the cross faults has been displaced 1 to 25 feet eastward.
Workings include 7,000 of development work by Lawler (1887-1892), by 1914 there were some 11,000 feet of workings, ultimately over 16,000 feet of workings. The shaft is 765 feet deep to the 1000 level. The vein was worked for 2,400 feet along the strike and stoped almost completely above the 700 level for an average length of 2,000 feet. Production included 58,748 oz. Au, 1,315,264 oz. Ag, 6,503,028 pounds Pb, 3,300,524 pounds Zn and 398,813 pounds of Cu. (to 1951).
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
| ⓘ Acanthite Formula: Ag2S Description: Small crystals on vuggy quartz. |
| ⓘ Andersonite (TL) Formula: Na2Ca(UO2)(CO3)3 · 5.33H2O Type Locality: Habit: Pseudo-cubic Colour: Bright yellow-green Fluorescence: Bright whitish-green Description: Occurs as an efflorescence on walls of mine workings. References: Axelrod, Joseph M., Grimaldi, Frank S., Milton, Charles, Murata, and K. J. (1951) The uranium minerals from the Hillside Mine, Yavapai County, Arizona. American Mineralogist, 36 (1-2) 1-22 |
| ⓘ Anglesite Formula: PbSO4 |
| ⓘ Arsenopyrite Formula: FeAsS Description: Small aggregates. |
| ⓘ Bayleyite (TL) Formula: Mg2(UO2)(CO3)3 · 18H2O Type Locality: Habit: Sharp, well-faceted Colour: sulphur-yellow Description: Occurs with schröckingerite and gypsum on 300 level north of the shaft. References: Axelrod, Joseph M., Grimaldi, Frank S., Milton, Charles, Murata, and K. J. (1951) The uranium minerals from the Hillside Mine, Yavapai County, Arizona. American Mineralogist, 36 (1-2) 1-22 |
| ⓘ Carnotite Formula: K2(UO2)2(VO4)2 · 3H2O |
| ⓘ Cerussite Formula: PbCO3 |
| ⓘ Chalcocite Formula: Cu2S Description: Small quantities. |
| ⓘ Chalcopyrite Formula: CuFeS2 |
| ⓘ Chlorargyrite Formula: AgCl Description: Locally abundant on upper levels in the oxidized zone. |
| ⓘ Covellite Formula: CuS Description: Coatings on sphalerite at base of oxidized zone. |
| ⓘ Fluorite Formula: CaF2 |
| ⓘ Galena Formula: PbS |
| ✪ Goslarite Formula: ZnSO4 · 7H2O Habit: Fibrous Colour: White Description: Silky fibers perpendicular to the drift walls, especially common in upper levels. |
| ⓘ Gypsum Formula: CaSO4 · 2H2O Description: Occurs in oxidized portion of the vein as efflorescent coatings associated with secondary uranium minerals; on the 300 level north of the shaft with schröckingerite and bayleyite. References: Axelrod, Joseph M., Grimaldi, Frank S., Milton, Charles, Murata, and K. J. (1951) The uranium minerals from the Hillside Mine, Yavapai County, Arizona. American Mineralogist, 36 (1-2) 1-22 |
| ⓘ Hemimorphite Formula: Zn4Si2O7(OH)2 · H2O Description: Occurs in oxidized zone of sulfide-bearing vein in mica schist. |
| ⓘ Hisingerite Formula: Fe3+2(Si2O5)(OH)4 · 2H2O Colour: Brownish-black Description: As dripstone deposits coating walls and forming pendants in the upper levels. Has conchoidal fracture, greasy luster, is isotropic with index of refraction of 1.595 ± .005. |
| ⓘ Johannite Formula: Cu(UO2)2(SO4)2(OH)2 · 8H2O |
| ⓘ Malachite Formula: Cu2(CO3)(OH)2 |
| ⓘ Muscovite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Muscovite var. Sericite Formula: KAl2(AlSi3O10)(OH)2 |
| ⓘ Native Silver Formula: Ag Description: Found in vugs on all levels of oxidized zone as wires or as arborescent bunches. |
| ⓘ Natrozippeite Formula: Na5(UO2)8(SO4)4O5(OH)3 · 12H2O |
| ⓘ Nickelzippeite Formula: Ni2(UO2)6(SO4)3(OH)10 · 16H2O |
| ⓘ Pharmacosiderite Formula: KFe3+4(AsO4)3(OH)4 · 6-7H2O Colour: Bright emerald-green Description: Found on one occasion in the oxidized zone. |
| ⓘ Pyrite Formula: FeS2 |
| ⓘ Quartz Formula: SiO2 Description: Vuggy. |
| ⓘ Schröckingerite Formula: NaCa3(UO2)(CO3)3(SO4)F · 10H2O Habit: Rosettes Colour: Green Description: Occurs as crusts to 1/8 inch thick on gypsum on the 300 level north of the shaft. Scattered rosettes with bayleyite. References: Axelrod, Joseph M., Grimaldi, Frank S., Milton, Charles, Murata, and K. J. (1951) The uranium minerals from the Hillside Mine, Yavapai County, Arizona. American Mineralogist, 36 (1-2) 1-22 |
| ⓘ Siderite Formula: FeCO3 Colour: Pinkish-gray Description: Occurs locally in the Hillside vein, usuaklly in close association with tetrahedrite. |
| ⓘ Siderite var. Manganese-bearing Siderite Formula: (Fe,Mn)CO3 Colour: Pinkish-gray Description: Occurs locally in the Hillside vein, usuaklly in close association with tetrahedrite. |
| ⓘ Smithsonite Formula: ZnCO3 Description: Occurs in the oxidized zone of sulfide-bearing veins in mica schist. |
| ⓘ Sphalerite Formula: ZnS |
| ⓘ Swartzite (TL) Formula: MgCa(UO2)(CO3)3 · 12H2O Type Locality: Habit: Prismatic Colour: Green Fluorescence: Bright yellow-green (UV) Description: Occurs as an efflorescence on walls intergrown with other uranium minerals and gypsum. References: Axelrod, Joseph M., Grimaldi, Frank S., Milton, Charles, Murata, and K. J. (1951) The uranium minerals from the Hillside Mine, Yavapai County, Arizona. American Mineralogist, 36 (1-2) 1-22 |
| ⓘ 'Tetrahedrite Subgroup' Formula: Cu6(Cu4C2+2)Sb4S12S Description: Small gray crystals attached to vuggy quartz. |
| ⓘ Uraninite Formula: UO2 |
| ⓘ Zinczippeite (TL) Formula: Zn(UO2)2(SO4)O2 · 3.5H2O Type Locality: Habit: Minute, curved Description: Occurs as shreads & minute, curved crystals. |
| ⓘ Zippeite Formula: K3(UO2)4(SO4)2O3(OH) · 3H2O |
List of minerals arranged by Strunz 10th Edition classification
| Group 1 - Elements | |||
|---|---|---|---|
| ⓘ | Native Silver | 1.AA.05 | Ag |
| Group 2 - Sulphides and Sulfosalts | |||
| ⓘ | Chalcocite | 2.BA.05 | Cu2S |
| ⓘ | Acanthite | 2.BA.35 | Ag2S |
| ⓘ | Covellite | 2.CA.05a | CuS |
| ⓘ | Sphalerite | 2.CB.05a | ZnS |
| ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
| ⓘ | Galena | 2.CD.10 | PbS |
| ⓘ | Pyrite | 2.EB.05a | FeS2 |
| ⓘ | Arsenopyrite | 2.EB.20 | FeAsS |
| ⓘ | 'Tetrahedrite Subgroup' | 2.GB.05 | Cu6(Cu4C2+2)Sb4S12S |
| Group 3 - Halides | |||
| ⓘ | Chlorargyrite | 3.AA.15 | AgCl |
| ⓘ | Fluorite | 3.AB.25 | CaF2 |
| Group 4 - Oxides and Hydroxides | |||
| ⓘ | Quartz | 4.DA.05 | SiO2 |
| ⓘ | Uraninite | 4.DL.05 | UO2 |
| ⓘ | Carnotite | 4.HB.05 | K2(UO2)2(VO4)2 · 3H2O |
| Group 5 - Nitrates and Carbonates | |||
| ⓘ | Siderite | 5.AB.05 | FeCO3 |
| ⓘ | Smithsonite | 5.AB.05 | ZnCO3 |
| ⓘ | Siderite var. Manganese-bearing Siderite | 5.AB.05 | (Fe,Mn)CO3 |
| ⓘ | Cerussite | 5.AB.15 | PbCO3 |
| ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
| ⓘ | Bayleyite (TL) | 5.ED.05 | Mg2(UO2)(CO3)3 · 18H2O |
| ⓘ | Swartzite (TL) | 5.ED.10 | MgCa(UO2)(CO3)3 · 12H2O |
| ⓘ | Andersonite (TL) | 5.ED.30 | Na2Ca(UO2)(CO3)3 · 5.33H2O |
| ⓘ | Schröckingerite | 5.EG.05 | NaCa3(UO2)(CO3)3(SO4)F · 10H2O |
| Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
| ⓘ | Anglesite | 7.AD.35 | PbSO4 |
| ⓘ | Goslarite | 7.CB.40 | ZnSO4 · 7H2O |
| ⓘ | Gypsum | 7.CD.40 | CaSO4 · 2H2O |
| ⓘ | Johannite | 7.EB.05 | Cu(UO2)2(SO4)2(OH)2 · 8H2O |
| ⓘ | Nickelzippeite | 7.EC.05 | Ni2(UO2)6(SO4)3(OH)10 · 16H2O |
| ⓘ | Natrozippeite | 7.EC.05 | Na5(UO2)8(SO4)4O5(OH)3 · 12H2O |
| ⓘ | Zinczippeite (TL) | 7.EC.05 | Zn(UO2)2(SO4)O2 · 3.5H2O |
| ⓘ | Zippeite | 7.EC.05 | K3(UO2)4(SO4)2O3(OH) · 3H2O |
| Group 8 - Phosphates, Arsenates and Vanadates | |||
| ⓘ | Pharmacosiderite | 8.DK.10 | KFe3+4(AsO4)3(OH)4 · 6-7H2O |
| Group 9 - Silicates | |||
| ⓘ | Hemimorphite | 9.BD.10 | Zn4Si2O7(OH)2 · H2O |
| ⓘ | Muscovite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | var. Sericite | 9.EC.15 | KAl2(AlSi3O10)(OH)2 |
| ⓘ | Hisingerite | 9.ED.10 | Fe3+2(Si2O5)(OH)4 · 2H2O |
List of minerals for each chemical element
| H | Hydrogen | |
|---|---|---|
| H | ⓘ Andersonite | Na2Ca(UO2)(CO3)3 · 5.33H2O |
| H | ⓘ Bayleyite | Mg2(UO2)(CO3)3 · 18H2O |
| H | ⓘ Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| H | ⓘ Goslarite | ZnSO4 · 7H2O |
| H | ⓘ Gypsum | CaSO4 · 2H2O |
| H | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
| H | ⓘ Hisingerite | Fe23+(Si2O5)(OH)4 · 2H2O |
| H | ⓘ Johannite | Cu(UO2)2(SO4)2(OH)2 · 8H2O |
| H | ⓘ Malachite | Cu2(CO3)(OH)2 |
| H | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| H | ⓘ Nickelzippeite | Ni2(UO2)6(SO4)3(OH)10 · 16H2O |
| H | ⓘ Pharmacosiderite | KFe43+(AsO4)3(OH)4 · 6-7H2O |
| H | ⓘ Schröckingerite | NaCa3(UO2)(CO3)3(SO4)F · 10H2O |
| H | ⓘ Natrozippeite | Na5(UO2)8(SO4)4O5(OH)3 · 12H2O |
| H | ⓘ Swartzite | MgCa(UO2)(CO3)3 · 12H2O |
| H | ⓘ Zinczippeite | Zn(UO2)2(SO4)O2 · 3.5H2O |
| H | ⓘ Zippeite | K3(UO2)4(SO4)2O3(OH) · 3H2O |
| H | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| C | Carbon | |
| C | ⓘ Andersonite | Na2Ca(UO2)(CO3)3 · 5.33H2O |
| C | ⓘ Bayleyite | Mg2(UO2)(CO3)3 · 18H2O |
| C | ⓘ Cerussite | PbCO3 |
| C | ⓘ Malachite | Cu2(CO3)(OH)2 |
| C | ⓘ Schröckingerite | NaCa3(UO2)(CO3)3(SO4)F · 10H2O |
| C | ⓘ Siderite | FeCO3 |
| C | ⓘ Smithsonite | ZnCO3 |
| C | ⓘ Swartzite | MgCa(UO2)(CO3)3 · 12H2O |
| C | ⓘ Siderite var. Manganese-bearing Siderite | (Fe,Mn)CO3 |
| O | Oxygen | |
| O | ⓘ Andersonite | Na2Ca(UO2)(CO3)3 · 5.33H2O |
| O | ⓘ Anglesite | PbSO4 |
| O | ⓘ Bayleyite | Mg2(UO2)(CO3)3 · 18H2O |
| O | ⓘ Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| O | ⓘ Cerussite | PbCO3 |
| O | ⓘ Goslarite | ZnSO4 · 7H2O |
| O | ⓘ Gypsum | CaSO4 · 2H2O |
| O | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
| O | ⓘ Hisingerite | Fe23+(Si2O5)(OH)4 · 2H2O |
| O | ⓘ Johannite | Cu(UO2)2(SO4)2(OH)2 · 8H2O |
| O | ⓘ Malachite | Cu2(CO3)(OH)2 |
| O | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Nickelzippeite | Ni2(UO2)6(SO4)3(OH)10 · 16H2O |
| O | ⓘ Pharmacosiderite | KFe43+(AsO4)3(OH)4 · 6-7H2O |
| O | ⓘ Quartz | SiO2 |
| O | ⓘ Schröckingerite | NaCa3(UO2)(CO3)3(SO4)F · 10H2O |
| O | ⓘ Siderite | FeCO3 |
| O | ⓘ Smithsonite | ZnCO3 |
| O | ⓘ Natrozippeite | Na5(UO2)8(SO4)4O5(OH)3 · 12H2O |
| O | ⓘ Swartzite | MgCa(UO2)(CO3)3 · 12H2O |
| O | ⓘ Uraninite | UO2 |
| O | ⓘ Zinczippeite | Zn(UO2)2(SO4)O2 · 3.5H2O |
| O | ⓘ Zippeite | K3(UO2)4(SO4)2O3(OH) · 3H2O |
| O | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| O | ⓘ Siderite var. Manganese-bearing Siderite | (Fe,Mn)CO3 |
| F | Fluorine | |
| F | ⓘ Fluorite | CaF2 |
| F | ⓘ Schröckingerite | NaCa3(UO2)(CO3)3(SO4)F · 10H2O |
| Na | Sodium | |
| Na | ⓘ Andersonite | Na2Ca(UO2)(CO3)3 · 5.33H2O |
| Na | ⓘ Schröckingerite | NaCa3(UO2)(CO3)3(SO4)F · 10H2O |
| Na | ⓘ Natrozippeite | Na5(UO2)8(SO4)4O5(OH)3 · 12H2O |
| Mg | Magnesium | |
| Mg | ⓘ Bayleyite | Mg2(UO2)(CO3)3 · 18H2O |
| Mg | ⓘ Swartzite | MgCa(UO2)(CO3)3 · 12H2O |
| Al | Aluminium | |
| Al | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Al | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Si | Silicon | |
| Si | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
| Si | ⓘ Hisingerite | Fe23+(Si2O5)(OH)4 · 2H2O |
| Si | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| Si | ⓘ Quartz | SiO2 |
| Si | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| S | Sulfur | |
| S | ⓘ Acanthite | Ag2S |
| S | ⓘ Anglesite | PbSO4 |
| S | ⓘ Arsenopyrite | FeAsS |
| S | ⓘ Chalcopyrite | CuFeS2 |
| S | ⓘ Chalcocite | Cu2S |
| S | ⓘ Covellite | CuS |
| S | ⓘ Galena | PbS |
| S | ⓘ Goslarite | ZnSO4 · 7H2O |
| S | ⓘ Gypsum | CaSO4 · 2H2O |
| S | ⓘ Johannite | Cu(UO2)2(SO4)2(OH)2 · 8H2O |
| S | ⓘ Nickelzippeite | Ni2(UO2)6(SO4)3(OH)10 · 16H2O |
| S | ⓘ Pyrite | FeS2 |
| S | ⓘ Schröckingerite | NaCa3(UO2)(CO3)3(SO4)F · 10H2O |
| S | ⓘ Natrozippeite | Na5(UO2)8(SO4)4O5(OH)3 · 12H2O |
| S | ⓘ Sphalerite | ZnS |
| S | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| S | ⓘ Zinczippeite | Zn(UO2)2(SO4)O2 · 3.5H2O |
| S | ⓘ Zippeite | K3(UO2)4(SO4)2O3(OH) · 3H2O |
| Cl | Chlorine | |
| Cl | ⓘ Chlorargyrite | AgCl |
| K | Potassium | |
| K | ⓘ Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| K | ⓘ Muscovite | KAl2(AlSi3O10)(OH)2 |
| K | ⓘ Pharmacosiderite | KFe43+(AsO4)3(OH)4 · 6-7H2O |
| K | ⓘ Zippeite | K3(UO2)4(SO4)2O3(OH) · 3H2O |
| K | ⓘ Muscovite var. Sericite | KAl2(AlSi3O10)(OH)2 |
| Ca | Calcium | |
| Ca | ⓘ Andersonite | Na2Ca(UO2)(CO3)3 · 5.33H2O |
| Ca | ⓘ Fluorite | CaF2 |
| Ca | ⓘ Gypsum | CaSO4 · 2H2O |
| Ca | ⓘ Schröckingerite | NaCa3(UO2)(CO3)3(SO4)F · 10H2O |
| Ca | ⓘ Swartzite | MgCa(UO2)(CO3)3 · 12H2O |
| V | Vanadium | |
| V | ⓘ Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| Mn | Manganese | |
| Mn | ⓘ Siderite var. Manganese-bearing Siderite | (Fe,Mn)CO3 |
| Fe | Iron | |
| Fe | ⓘ Arsenopyrite | FeAsS |
| Fe | ⓘ Chalcopyrite | CuFeS2 |
| Fe | ⓘ Hisingerite | Fe23+(Si2O5)(OH)4 · 2H2O |
| Fe | ⓘ Pharmacosiderite | KFe43+(AsO4)3(OH)4 · 6-7H2O |
| Fe | ⓘ Pyrite | FeS2 |
| Fe | ⓘ Siderite | FeCO3 |
| Fe | ⓘ Siderite var. Manganese-bearing Siderite | (Fe,Mn)CO3 |
| Ni | Nickel | |
| Ni | ⓘ Nickelzippeite | Ni2(UO2)6(SO4)3(OH)10 · 16H2O |
| Cu | Copper | |
| Cu | ⓘ Chalcopyrite | CuFeS2 |
| Cu | ⓘ Chalcocite | Cu2S |
| Cu | ⓘ Covellite | CuS |
| Cu | ⓘ Johannite | Cu(UO2)2(SO4)2(OH)2 · 8H2O |
| Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
| Cu | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Zn | Zinc | |
| Zn | ⓘ Goslarite | ZnSO4 · 7H2O |
| Zn | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
| Zn | ⓘ Smithsonite | ZnCO3 |
| Zn | ⓘ Sphalerite | ZnS |
| Zn | ⓘ Zinczippeite | Zn(UO2)2(SO4)O2 · 3.5H2O |
| As | Arsenic | |
| As | ⓘ Arsenopyrite | FeAsS |
| As | ⓘ Pharmacosiderite | KFe43+(AsO4)3(OH)4 · 6-7H2O |
| Ag | Silver | |
| Ag | ⓘ Acanthite | Ag2S |
| Ag | ⓘ Chlorargyrite | AgCl |
| Ag | ⓘ Native Silver | Ag |
| Sb | Antimony | |
| Sb | ⓘ Tetrahedrite Subgroup | Cu6(Cu4C22+)Sb4S12S |
| Pb | Lead | |
| Pb | ⓘ Anglesite | PbSO4 |
| Pb | ⓘ Cerussite | PbCO3 |
| Pb | ⓘ Galena | PbS |
| U | Uranium | |
| U | ⓘ Andersonite | Na2Ca(UO2)(CO3)3 · 5.33H2O |
| U | ⓘ Bayleyite | Mg2(UO2)(CO3)3 · 18H2O |
| U | ⓘ Carnotite | K2(UO2)2(VO4)2 · 3H2O |
| U | ⓘ Johannite | Cu(UO2)2(SO4)2(OH)2 · 8H2O |
| U | ⓘ Nickelzippeite | Ni2(UO2)6(SO4)3(OH)10 · 16H2O |
| U | ⓘ Schröckingerite | NaCa3(UO2)(CO3)3(SO4)F · 10H2O |
| U | ⓘ Natrozippeite | Na5(UO2)8(SO4)4O5(OH)3 · 12H2O |
| U | ⓘ Swartzite | MgCa(UO2)(CO3)3 · 12H2O |
| U | ⓘ Uraninite | UO2 |
| U | ⓘ Zinczippeite | Zn(UO2)2(SO4)O2 · 3.5H2O |
| U | ⓘ Zippeite | K3(UO2)4(SO4)2O3(OH) · 3H2O |
Other Regions, Features and Areas containing this locality
North AmericaContinent
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Mojave DomainDomain
- Southern Basin and RangeWide Rift
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References
Axelrod, Joseph M., Grimaldi, Frank S., Milton, Charles, Murata, and K. J. (1951) The uranium minerals from the Hillside Mine, Yavapai County, Arizona. American Mineralogist, 36 (1-2) 1-22
Frondel, Clifford (1958) Systematic mineralogy of uranium and thorium. Bulletin 1064. US Geological Survey doi:10.3133/b1064
Anthony, John W.; Williams, Sidney A.; Bideaux, Richard A.; Grant, Raymond W. (1995) Mineralogy of Arizona (3rd ed.). University of Arizona Press.pages 111-112, 130, 155, 159, 170, 229, 242, 248, 263, 313, 365, 375, 387, 407, 430
Hillside Mine, Bozarth Mesa, Bagdad, Eureka Mining District, Yavapai County, Arizona, USA