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Copper Giant claims, New Cornelia Mine area, New Cornelia Mine, Ajo, Little Ajo Mountains, Ajo Mining District, Pima County, Arizona, USAi
Regional Level Types
Copper Giant claimsGroup of Claims
New Cornelia Mine areaMining Area
New Cornelia MineMine (Inactive)
AjoCensus-designated Place
Little Ajo MountainsMountain Range
Ajo Mining DistrictMining District
Pima CountyCounty
ArizonaState
USACountry

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Latitude & Longitude (WGS84):
32° 17' 56'' North , 112° 52' 14'' West
Latitude & Longitude (decimal):
Type:
Group of Claims
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Ajo3,304 (2011)8.1km
Why167 (2017)12.8km
Colinas de Sonoidag289 (2014)46.2km
Adolfo López Mateos201 (2014)48.6km
Sonoita12,849 (2018)48.6km
Mindat Locality ID:
46790
Long-form identifier:
mindat:1:2:46790:7
GUID (UUID V4):
0
Other/historical names associated with this locality:
Copper Giant deposits; Copper Giant group; Jumbo group; Greenway-Albert property


A group of 25 unpatented Cu-Fe claims located in secs. 10, 11 & the NE¼ sec. 15, T.13S., R.6W. (Ajo 15 minute topo map), on 26 claims. about 5 miles South of Ajo, at about 1,775 feet of altitude. Idle after 1942. Owned by Lotta I. Hunter, Pasadena, CA with J.H. Greenway Albert, Tombstone, AZ, as a lessee and holder of an option to purchase (circa 1952). Knox-Arizona Mining Co., owner, 1979.

Mineralization is bedded tabular ore bodies of secondary copper eroded from oxidized copper deposits to form clastic deposits within fanglomerate, or ground-water percolation dissolved clastic copper and later precipitated chrysocolla along favorable horizons. Slica also precipitated with copper.

Local rocks are the Locomotive Fanglomerate and the Ajo volcanics. Throughout this area small, scattered outcrops of copper mineralization, primarily chrysocolla, occur.

In the Copper Giant area, the Locomotive fanglomerate consists of many types of rock fragments in a red arkosic siltstone or sandstone matrix. The fragments are composed of monzonite, quartz monzonite, trachyte, pegmatite granite, diorite, schist and gneiss, andesite, limestone and dolomite, quartzite, and conglomerate. The Ajo volcanics interfinger with the fanglomerate, and some beds consist of a mixture of volcanic and non-volcanic fragments.

The volcanics in the area consist of andesitic breccias and tuffs, with little or no lava. The breccias consist of angular to subrounded fragments of gray to red andesite, vesicular andesite containing some amygdules filled with calcite, andesite containing phenocrysts of plagioclase 1 to 3 mm wide, and a small amount of diorite.
The mineralization at the surface is found along definite beds, mainly in the fanglomerate, and in irregular mineralized masses in the volcanics. There are 4 main zones in the fanglomerate. The largest of these can be followed for over 500 feet and varies in width from ½ to 7 feet. Another such zone, a few feet NE of the largest, can be followed for 400 feet and varies in width from ½ foot to 5 feet.

The surface showing may grade with depth to chalcocite. The ore is 152.4 meters long and 2.13 meters wide.

Workings are 12.19 meters deep.

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List

Mineral list contains entries from the region specified including sub-localities

6 valid minerals.

Detailed Mineral List:

ⓘ Calcite
Formula: CaCO3
Description: Occurs as vesicle fillings in drill cores.
ⓘ Chalcocite
Formula: Cu2S
ⓘ 'Chlorite Group'
ⓘ Chrysocolla
Formula: Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Description: The most abundant copper mineral that occurs fanglomerate & volcanic rocks, associated with a small amount of malachite, as grains ranging from less than 1 mm to 10 mm & as vein filling in small fractures and long joints.
ⓘ Epidote
Formula: (CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Description: In drill cores with specularite.
ⓘ Hematite
Formula: Fe2O3
Description: Some noted.
ⓘ Hematite var. Specularite
Formula: Fe2O3
Description: Some noted.
ⓘ Malachite
Formula: Cu2(CO3)(OH)2
Description: Occurs in small amounts in fanglomerate & volcanic rocks, associated with chrysocolla, as grains ranging from less than 1 mm to 10 mm & as vein filling in small fractures and long joints.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 2 - Sulphides and Sulfosalts
ⓘChalcocite2.BA.05Cu2S
Group 4 - Oxides and Hydroxides
ⓘHematite4.CB.05Fe2O3
ⓘvar. Specularite4.CB.05Fe2O3
Group 5 - Nitrates and Carbonates
ⓘCalcite5.AB.05CaCO3
ⓘMalachite5.BA.10Cu2(CO3)(OH)2
Group 9 - Silicates
ⓘEpidote9.BG.05a(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
ⓘChrysocolla9.ED.20Cu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Unclassified
ⓘ'Chlorite Group'-

List of minerals for each chemical element

HHydrogen
Hⓘ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Hⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Hⓘ MalachiteCu2(CO3)(OH)2
CCarbon
Cⓘ CalciteCaCO3
Cⓘ MalachiteCu2(CO3)(OH)2
OOxygen
Oⓘ CalciteCaCO3
Oⓘ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Oⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Oⓘ HematiteFe2O3
Oⓘ MalachiteCu2(CO3)(OH)2
Oⓘ Hematite var. SpeculariteFe2O3
AlAluminium
Alⓘ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Alⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
SiSilicon
Siⓘ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Siⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
SSulfur
Sⓘ ChalcociteCu2S
CaCalcium
Caⓘ CalciteCaCO3
Caⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
FeIron
Feⓘ Epidote(CaCa)(AlAlFe3+)O[Si2O7][SiO4](OH)
Feⓘ HematiteFe2O3
Feⓘ Hematite var. SpeculariteFe2O3
CuCopper
Cuⓘ ChalcociteCu2S
Cuⓘ ChrysocollaCu2-xAlx(H2-xSi2O5)(OH)4 · nH2O, x < 1
Cuⓘ MalachiteCu2(CO3)(OH)2

Other Databases

Link to USGS MRDS:10027149

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