Grand Wash Cliffs, Mohave County, Arizona, USAi
Regional Level Types | |
---|---|
Grand Wash Cliffs | Cliff |
Mohave County | County |
Arizona | State |
USA | Country |
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Latitude & Longitude (WGS84):
35° 58' 59'' North , 113° 58' 2'' West
Latitude & Longitude (decimal):
Locality type:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Meadview | 1,224 (2011) | 9.3km |
White Hills | 323 (2011) | 47.4km |
Dolan Springs | 2,033 (2011) | 51.5km |
Truxton | 134 (2011) | 66.3km |
Other/historical names associated with this locality:
Grand Cliff Range; Grand Wash Escarpment; Grand Wash Fault; Lower Grand Wash Cliffs; Lower Grand Wash Ledge
Named for the Grand Wash Trough which was formed by the "faulting and tilting of a large crust block" (US-T121) "faulting and tilting of a large crust block" (US-T121). The cliffs rise like steps from the lowland area to the high plateaus. The north end is at 363130N 1134700W. The south end is at 352300N 1134200W. plateaus: The north end is at 363130N 1134700W. The south end is at 352300N 1134200W. This locality is not listed in the USGS MRDS database.
GRAND WASH CLIFFS.
The Grand Wash Cliffs constitute the great break of the Colorado Plateau into the Great Basin. They undoubtedly represent a fault line, as has been described by previous writers, and are so shown on the accompanying map (Plate I). Dutton describes the Grand Wash fault as a gigantic displacement in which the whole country to the west has dropped down 6,000 or 7,000 feet. This fault is best developed along the edge of the plateau, extending from the mouth of the Grand Canyon southeastward to Music Mountain, a distance of about 50 miles, with a height of escarpment of about 3,000 feet and an average width of about 3 miles. The regularity of its course is locally interrupted by embayments or short, deep canyons cut back into the plateau, the most marked example being that at Clay Spring, north of Music Mountain camp.
From the edge of the plateau the general trend of the slope is westsouthwest into Hualpai Valley. Typically this slope is made up of three topographic elements; these are, in descending order, (1) an upper; more or less precipitous cliff or scarp, a-bout 1,500 feet in height, composed of the nearly horizontal strata of the Grand Canyon section; (2) an intermediate mountainous belt, in many places steep and rugged, composed of pre-Cambrian rocks having a vertical range of 1,000 or more feet and a breadth of about 2 miles; (3) a less steep foothill belt of irregular hills and ridges, consisting of similar granitoid rocks, which, with immense local deposits or fans of steep-lying talus or coarse, mostly granitoid, debris, descend from 600 to 1,000 feet to the edge of the valley.
At Music Mountain the Grand Wash Cliffs divide, the upper or sedimentary portion extending eastward under the name of Yampai Cliffs, and the lower or crystalline portion continuing southward under the names of Cottonwood Cliffs and Aquarius Cliffs, forming the edge of the Truxton Plateau.
The Grand Wash Cliffs constitute the great break of the Colorado Plateau into the Great Basin. They undoubtedly represent a fault line, as has been described by previous writers, and are so shown on the accompanying map (Plate I). Dutton describes the Grand Wash fault as a gigantic displacement in which the whole country to the west has dropped down 6,000 or 7,000 feet. This fault is best developed along the edge of the plateau, extending from the mouth of the Grand Canyon southeastward to Music Mountain, a distance of about 50 miles, with a height of escarpment of about 3,000 feet and an average width of about 3 miles. The regularity of its course is locally interrupted by embayments or short, deep canyons cut back into the plateau, the most marked example being that at Clay Spring, north of Music Mountain camp.
From the edge of the plateau the general trend of the slope is westsouthwest into Hualpai Valley. Typically this slope is made up of three topographic elements; these are, in descending order, (1) an upper; more or less precipitous cliff or scarp, a-bout 1,500 feet in height, composed of the nearly horizontal strata of the Grand Canyon section; (2) an intermediate mountainous belt, in many places steep and rugged, composed of pre-Cambrian rocks having a vertical range of 1,000 or more feet and a breadth of about 2 miles; (3) a less steep foothill belt of irregular hills and ridges, consisting of similar granitoid rocks, which, with immense local deposits or fans of steep-lying talus or coarse, mostly granitoid, debris, descend from 600 to 1,000 feet to the edge of the valley.
At Music Mountain the Grand Wash Cliffs divide, the upper or sedimentary portion extending eastward under the name of Yampai Cliffs, and the lower or crystalline portion continuing southward under the names of Cottonwood Cliffs and Aquarius Cliffs, forming the edge of the Truxton Plateau.
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Rock Types Recorded
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Alphabetical List Tree DiagramDetailed Mineral List:
ⓘ Albite Formula: Na(AlSi3O8) Reference: Schrader, F.C. (1909), Mineral deposits of the Cerbat Range, Black Mountains, and Grand Wash Cliffs, Mohave County, Arizona, USGS Bulletin 397: 142-144. |
ⓘ Albite var. Andesine Formula: (Na,Ca)[Al(Si,Al)Si2O8] Reference: Schrader, F.C. (1909), Mineral deposits of the Cerbat Range, Black Mountains, and Grand Wash Cliffs, Mohave County, Arizona, USGS Bulletin 397: 142-144. |
ⓘ Albite var. Oligoclase Formula: (Na,Ca)[Al(Si,Al)Si2O8] Reference: Schrader, F.C. (1909), Mineral deposits of the Cerbat Range, Black Mountains, and Grand Wash Cliffs, Mohave County, Arizona, USGS Bulletin 397: 142-144. |
ⓘ Andalusite Formula: Al2(SiO4)O Description: Occurs in pegmatite. Reference: Galbraith, F.W. & Brennan (1959), Minerals of AZ: 28, 98. |
ⓘ Azurite Formula: Cu3(CO3)2(OH)2 Localities: Savanic Mine (Bronzel Mine; Bronze L Mine), Grand Gulch Bench, Bentley Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Copper Mountain Mine (Copper King Mine), Bentley Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Grand Gulch Mine, Bentley Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd. ed.: 126; Hill, J.M. (1914b), The Grand Gulch Mining region, Mohave Co., AZ, USGS Bull. 580: 39-58.. |
ⓘ 'Biotite' Formula: K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 Reference: Schrader, F.C. (1909), Mineral deposits of the Cerbat Range, Black Mountains, and Grand Wash Cliffs, Mohave County, Arizona, USGS Bulletin 397: 142-144. |
ⓘ Bornite Formula: Cu5FeS4 Localities: Reference: Galbraith, F.W. (1947), AZ Bur. of mines Bull. 153, Minerals of AZ: 17; MRDS file #10027690. |
ⓘ Brochantite Formula: Cu4(SO4)(OH)6 Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd. ed.: 146; Hill, J.M. (1914b), The Grand Gulch Mining Region, Mohave Co., AZ, USGS Bull.580: 39-58; Galbraith, F.W. & Brennan (1959), Mineras of AZ: 63. |
ⓘ Calcite Formula: CaCO3 Localities: Reference: MRDS file #10027690. |
ⓘ Chalcocite Formula: Cu2S Localities: Savanic Mine (Bronzel Mine; Bronze L Mine), Grand Gulch Bench, Bentley Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Copper Mountain Mine (Copper King Mine), Bentley Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Grand Gulch Mine, Bentley Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd. ed.: 163; Hill, J.M. (1914b), The Grand Gulch Mining region, Mohave Co., AZ, USGS Bull. 580: 39-58; Galbraith, F.W. (1947), AZ Bur. of Mines Bull. 153, Minerals of AZ: 16; MRDS file #10027690. |
ⓘ Chalcopyrite Formula: CuFeS2 Localities: Reference: Galbraith, F.W. (1947), AZ Bur. of mines Bull. 153, Minerals of AZ: 19; MRDS file #10027690. |
ⓘ Chrysocolla Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 Reference: MRDS file #10102539. |
ⓘ Corundum Formula: Al2O3 Colour: Blue, red, white Description: Associated with andalusite in an aluminous pegmatite dike. Reference: Galbraith, F.W. & Brennan (1959), Minerals of AZ: 28. |
ⓘ Cotunnite Formula: PbCl2 Description: Reported as small veinlets replacing chalcocite. Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd. ed.: 190; Hill, J.M. (1914b), The Grand Gulch Mining Region, Mohave Co., AZ, USGS Bull.580: 39-58; Galbraith, F.W. & Brennan (1959), Mineras of AZ: 44. |
ⓘ Cuprite Formula: Cu2O Localities: Reference: MRDS file #10027660. |
ⓘ Descloizite Formula: PbZn(VO4)(OH) Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd. ed.: 201; Hill, J.M. (1914b), The Grand Gulch Mining Region, Mohave Co., AZ, USGS Bull.580: 39-58; Galbraith, F.W. & Brennan (1959), Mineras of AZ: 70. |
ⓘ Descloizite var. Copper-bearing Descloizite Formula: Pb(Zn,Cu)VO4OH Reference: MRDS file #10102539. |
ⓘ Dolomite Formula: CaMg(CO3)2 Reference: MRDS file #10027690. |
ⓘ Galena Formula: PbS Localities: Ellen Jane Mine, Camp Wash, Music Mountain Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Grand Wash Cliffs, Mohave County, Arizona, USA Music Mountain Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Music Mountain Mine group (Lucknow Mine), Music Mountain Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Reference: Wilson, E.D., et al (1934), AZ Bur. of Mines Bull. 137: 109. |
ⓘ Gold Formula: Au Localities: Reference: Wilson, E.D., et al (1934), AZ Bur. of Mines Bull. 137: 108-109. |
ⓘ Hematite Formula: Fe2O3 Reference: Econ Geol (1985) 80:1722-1735 |
ⓘ Hemimorphite Formula: Zn4Si2O7(OH)2 · H2O Reference: Econ Geol (1985) 80:1722-1735 |
ⓘ Malachite Formula: Cu2(CO3)(OH)2 Localities: Savanic Mine (Bronzel Mine; Bronze L Mine), Grand Gulch Bench, Bentley Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Copper Mountain Mine (Copper King Mine), Bentley Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Copper House Mine (Copper House Coalition #2 Mine), Bentley Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Grand Gulch Mine, Bentley Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Reference: Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd. ed.: 286; Hill, J.M. (1914b), The Grand Gulch Mining region, Mohave Co., AZ, USGS Bull. 580: 39-58; MRDS file #10027690. |
ⓘ Microcline Formula: K(AlSi3O8) Reference: Schrader, F.C. (1909), Mineral deposits of the Cerbat Range, Black Mountains, and Grand Wash Cliffs, Mohave County, Arizona, USGS Bulletin 397: 142-144. |
ⓘ Orthoclase Formula: K(AlSi3O8) Reference: Schrader, F.C. (1909), Mineral deposits of the Cerbat Range, Black Mountains, and Grand Wash Cliffs, Mohave County, Arizona, USGS Bulletin 397: 142-144. |
ⓘ Pyrite Formula: FeS2 Localities: Ellen Jane Mine, Camp Wash, Music Mountain Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Music Mountain Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Music Mountain Mine group (Lucknow Mine), Music Mountain Mining District, Grand Wash Cliffs, Mohave County, Arizona, USA Reference: Wilson, E.D., et al (1934), AZ Bur. of Mines Bull. 137: 109. |
ⓘ Quartz Formula: SiO2 Localities: Reference: Wilson, E.D., et al (1934), Arizona Bureau of Mines Bulletin 137: 109. |
ⓘ Smithsonite Formula: ZnCO3 Reference: Econ Geol (1985) 80:1722-1735 |
ⓘ Tenorite Formula: CuO Reference: Copper Handbook 1911 |
ⓘ Uraninite Formula: UO2 Reference: MRDS file #10027660. |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 1 - Elements | |||
---|---|---|---|
ⓘ | Gold | 1.AA.05 | Au |
Group 2 - Sulphides and Sulfosalts | |||
ⓘ | Bornite | 2.BA.15 | Cu5FeS4 |
ⓘ | Chalcocite | 2.BA.05 | Cu2S |
ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
ⓘ | Galena | 2.CD.10 | PbS |
ⓘ | Pyrite | 2.EB.05a | FeS2 |
Group 3 - Halides | |||
ⓘ | Cotunnite | 3.AB.85 | PbCl2 |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Corundum | 4.CB.05 | Al2O3 |
ⓘ | Cuprite | 4.AA.10 | Cu2O |
ⓘ | Hematite | 4.CB.05 | Fe2O3 |
ⓘ | Quartz | 4.DA.05 | SiO2 |
ⓘ | Tenorite | 4.AB.10 | CuO |
ⓘ | Uraninite | 4.DL.05 | UO2 |
Group 5 - Nitrates and Carbonates | |||
ⓘ | Azurite | 5.BA.05 | Cu3(CO3)2(OH)2 |
ⓘ | Calcite | 5.AB.05 | CaCO3 |
ⓘ | Dolomite | 5.AB.10 | CaMg(CO3)2 |
ⓘ | Malachite | 5.BA.10 | Cu2(CO3)(OH)2 |
ⓘ | Smithsonite | 5.AB.05 | ZnCO3 |
Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
ⓘ | Brochantite | 7.BB.25 | Cu4(SO4)(OH)6 |
Group 8 - Phosphates, Arsenates and Vanadates | |||
ⓘ | Descloizite | 8.BH.40 | PbZn(VO4)(OH) |
ⓘ | var. Copper-bearing Descloizite | 8.BH.40 | Pb(Zn,Cu)VO4OH |
Group 9 - Silicates | |||
ⓘ | Albite | 9.FA.35 | Na(AlSi3O8) |
ⓘ | var. Andesine | 9.FA.35 | (Na,Ca)[Al(Si,Al)Si2O8] |
ⓘ | var. Oligoclase | 9.FA.35 | (Na,Ca)[Al(Si,Al)Si2O8] |
ⓘ | Andalusite | 9.AF.10 | Al2(SiO4)O |
ⓘ | Chrysocolla | 9.ED.20 | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
ⓘ | Hemimorphite | 9.BD.10 | Zn4Si2O7(OH)2 · H2O |
ⓘ | Microcline | 9.FA.30 | K(AlSi3O8) |
ⓘ | Orthoclase | 9.FA.30 | K(AlSi3O8) |
Unclassified Minerals, Rocks, etc. | |||
ⓘ | 'Biotite' | - | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Azurite | Cu3(CO3)2(OH)2 |
H | ⓘ Malachite | Cu2(CO3)(OH)2 |
H | ⓘ Brochantite | Cu4(SO4)(OH)6 |
H | ⓘ Descloizite | PbZn(VO4)(OH) |
H | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
H | ⓘ Descloizite var. Copper-bearing Descloizite | Pb(Zn,Cu)VO4OH |
H | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
H | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
C | Carbon | |
C | ⓘ Azurite | Cu3(CO3)2(OH)2 |
C | ⓘ Malachite | Cu2(CO3)(OH)2 |
C | ⓘ Dolomite | CaMg(CO3)2 |
C | ⓘ Calcite | CaCO3 |
C | ⓘ Smithsonite | ZnCO3 |
O | Oxygen | |
O | ⓘ Azurite | Cu3(CO3)2(OH)2 |
O | ⓘ Malachite | Cu2(CO3)(OH)2 |
O | ⓘ Brochantite | Cu4(SO4)(OH)6 |
O | ⓘ Descloizite | PbZn(VO4)(OH) |
O | ⓘ Andalusite | Al2(SiO4)O |
O | ⓘ Corundum | Al2O3 |
O | ⓘ Uraninite | UO2 |
O | ⓘ Cuprite | Cu2O |
O | ⓘ Dolomite | CaMg(CO3)2 |
O | ⓘ Calcite | CaCO3 |
O | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
O | ⓘ Descloizite var. Copper-bearing Descloizite | Pb(Zn,Cu)VO4OH |
O | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
O | ⓘ Smithsonite | ZnCO3 |
O | ⓘ Hematite | Fe2O3 |
O | ⓘ Tenorite | CuO |
O | ⓘ Albite var. Oligoclase | (Na,Ca)[Al(Si,Al)Si2O8] |
O | ⓘ Microcline | K(AlSi3O8) |
O | ⓘ Orthoclase | K(AlSi3O8) |
O | ⓘ Albite var. Andesine | (Na,Ca)[Al(Si,Al)Si2O8] |
O | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
O | ⓘ Albite | Na(AlSi3O8) |
O | ⓘ Quartz | SiO2 |
F | Fluorine | |
F | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Na | Sodium | |
Na | ⓘ Albite var. Oligoclase | (Na,Ca)[Al(Si,Al)Si2O8] |
Na | ⓘ Albite var. Andesine | (Na,Ca)[Al(Si,Al)Si2O8] |
Na | ⓘ Albite | Na(AlSi3O8) |
Mg | Magnesium | |
Mg | ⓘ Dolomite | CaMg(CO3)2 |
Mg | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Al | Aluminium | |
Al | ⓘ Andalusite | Al2(SiO4)O |
Al | ⓘ Corundum | Al2O3 |
Al | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
Al | ⓘ Albite var. Oligoclase | (Na,Ca)[Al(Si,Al)Si2O8] |
Al | ⓘ Microcline | K(AlSi3O8) |
Al | ⓘ Orthoclase | K(AlSi3O8) |
Al | ⓘ Albite var. Andesine | (Na,Ca)[Al(Si,Al)Si2O8] |
Al | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Al | ⓘ Albite | Na(AlSi3O8) |
Si | Silicon | |
Si | ⓘ Andalusite | Al2(SiO4)O |
Si | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
Si | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
Si | ⓘ Albite var. Oligoclase | (Na,Ca)[Al(Si,Al)Si2O8] |
Si | ⓘ Microcline | K(AlSi3O8) |
Si | ⓘ Orthoclase | K(AlSi3O8) |
Si | ⓘ Albite var. Andesine | (Na,Ca)[Al(Si,Al)Si2O8] |
Si | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Si | ⓘ Albite | Na(AlSi3O8) |
Si | ⓘ Quartz | SiO2 |
S | Sulfur | |
S | ⓘ Bornite | Cu5FeS4 |
S | ⓘ Chalcocite | Cu2S |
S | ⓘ Chalcopyrite | CuFeS2 |
S | ⓘ Pyrite | FeS2 |
S | ⓘ Galena | PbS |
S | ⓘ Brochantite | Cu4(SO4)(OH)6 |
Cl | Chlorine | |
Cl | ⓘ Cotunnite | PbCl2 |
K | Potassium | |
K | ⓘ Microcline | K(AlSi3O8) |
K | ⓘ Orthoclase | K(AlSi3O8) |
K | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Ca | Calcium | |
Ca | ⓘ Dolomite | CaMg(CO3)2 |
Ca | ⓘ Calcite | CaCO3 |
Ca | ⓘ Albite var. Oligoclase | (Na,Ca)[Al(Si,Al)Si2O8] |
Ca | ⓘ Albite var. Andesine | (Na,Ca)[Al(Si,Al)Si2O8] |
Ti | Titanium | |
Ti | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
V | Vanadium | |
V | ⓘ Descloizite | PbZn(VO4)(OH) |
V | ⓘ Descloizite var. Copper-bearing Descloizite | Pb(Zn,Cu)VO4OH |
Fe | Iron | |
Fe | ⓘ Bornite | Cu5FeS4 |
Fe | ⓘ Chalcopyrite | CuFeS2 |
Fe | ⓘ Pyrite | FeS2 |
Fe | ⓘ Hematite | Fe2O3 |
Fe | ⓘ Biotite | K(Fe2+/Mg)2(Al/Fe3+/Mg/Ti)([Si/Al/Fe]2Si2O10)(OH/F)2 or Simplified: K(Mg,Fe)3AlSi3O10(OH)2 |
Cu | Copper | |
Cu | ⓘ Azurite | Cu3(CO3)2(OH)2 |
Cu | ⓘ Bornite | Cu5FeS4 |
Cu | ⓘ Chalcocite | Cu2S |
Cu | ⓘ Chalcopyrite | CuFeS2 |
Cu | ⓘ Malachite | Cu2(CO3)(OH)2 |
Cu | ⓘ Brochantite | Cu4(SO4)(OH)6 |
Cu | ⓘ Cuprite | Cu2O |
Cu | ⓘ Chrysocolla | Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1 |
Cu | ⓘ Descloizite var. Copper-bearing Descloizite | Pb(Zn,Cu)VO4OH |
Cu | ⓘ Tenorite | CuO |
Zn | Zinc | |
Zn | ⓘ Descloizite | PbZn(VO4)(OH) |
Zn | ⓘ Descloizite var. Copper-bearing Descloizite | Pb(Zn,Cu)VO4OH |
Zn | ⓘ Hemimorphite | Zn4Si2O7(OH)2 · H2O |
Zn | ⓘ Smithsonite | ZnCO3 |
Au | Gold | |
Au | ⓘ Gold | Au |
Pb | Lead | |
Pb | ⓘ Galena | PbS |
Pb | ⓘ Cotunnite | PbCl2 |
Pb | ⓘ Descloizite | PbZn(VO4)(OH) |
Pb | ⓘ Descloizite var. Copper-bearing Descloizite | Pb(Zn,Cu)VO4OH |
U | Uranium | |
U | ⓘ Uraninite | UO2 |
References
Sort by
Year (asc) Year (desc) Author (A-Z) Author (Z-A) In-text Citation No. Schrader, F.C. (1909), The Mineral deposits of the Cerbat Range, Black Mountains, and Grand Wash Cliffs, Mohave County, Arizona, USGS Bulletin 397: 18-19.
Thomas, B.E. (1949), Ore deposits of the Wallapai District, Arizona, Economic Geology: 44: 663-705.
Galbraith, F.W. & Brennan (1959), Minerals of Arizona: 28, 98.
Albin, Alton L. (1991), Geologic map of the Peacock Mountains and Southern Grand Wash Cliffs: including Peacock Peak, Antares, Hackberry, Valentine, and the Southern Half of the Music Mountain SE, and Milkweed Canyon SW, 1/2 Minute Quadrangles, Northwestern Arizona, Arizona Geological Survey CM-91K, 1:24000 scale.
Anthony, J.W., et al (1995), Mineralogy of Arizona, 3rd. edition: 228.
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