Black Mesa Mine (Black Mesa breccia pipe), Black Mesa, Eureka Mining District, Yavapai County, Arizona, USAi
Regional Level Types | |
---|---|
Black Mesa Mine (Black Mesa breccia pipe) | Mine |
Black Mesa | Mesa |
Eureka Mining District | Mining District |
Yavapai County | County |
Arizona | State |
USA | Country |
This page is currently not sponsored. Click here to sponsor this page.
Latitude & Longitude (WGS84):
34° 35' 32'' North , 113° 13' 0'' West
Latitude & Longitude (decimal):
Type:
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Bagdad | 1,876 (2016) | 1.7km |
Wikieup | 133 (2011) | 38.1km |
Peeples Valley | 428 (2011) | 57.5km |
Congress | 1,975 (2014) | 58.4km |
Yarnell | 649 (2011) | 59.6km |
Mindat Locality ID:
61233
Long-form identifier:
mindat:1:2:61233:0
GUID (UUID V4):
e71fc810-294e-40f7-b1e3-cbec7a771a5e
A Cu-Mo breccia pipe deposit with underground workings located on the east side of Copper Creek, less than 1 mile to the north of the Bagdad Mine. Owned by the Bagdad Copper Corp.
Mineralization is a breccia pipe hosted in the Butte Falls Tuff and King Peak Rhyolite. Ore control was faulting and shearing. No alteration noted.
The fragments are largely of quartz monzonite, though some may be of diorite porphyry, but the fragments are so sericitized and silicified that original textures cannot be recognized with certainty in most specimens. The fragments range from 1 inch (2.5 cm) to 1 foot (30 cm) across and they are cemented by irregular vuggy quartz veins to 2 inches (5 cm) wide.
The sulfide minerals are confined largely to the vuggy quartz veins; and pyrite and chalcopyrite crystals nest in the vugs, the smaller grains are embedded in the quartz. Fine, flaky molybdenite crystals are distributed sporadically through the breccia, appearing mostly at the margins of the cementing quartz veins, but a few flakes appear in the vugs. Small veinlets of quartz cut the altered quartz monzonite fragments and carry three sulfides in variable distribution.
The sulfide mineralization is somewhat sporadic; the largest and most abundant chalcopyrite crystals appear at the western margin of the pipe. The only copper carbonate appears where the Hawkeye fault cuts the pipe.
The breccia is heavily coated with chalcanthite along the adit walls for the first 100 feet. A little antlerite was also observed.
Area structures include foliation in metavolcanic rocks that trends N10E to N40E.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
ⓘ Antlerite Formula: Cu3(SO4)(OH)4 Description: Occurs in the walls of the adit with chalcanthite. |
ⓘ Chalcanthite Formula: CuSO4 · 5H2O Description: Crusts on working walls attaining tbhicknesses of 2 to 3 inches (5 to 7.5 cm). |
ⓘ Chalcocite Formula: Cu2S Description: Coatings on chalcopyrite. |
ⓘ Chalcopyrite Formula: CuFeS2 |
ⓘ 'Limonite' Colour: Maroon; reddish-brown Description: Fluffy maroon material derived from chalcocite. |
ⓘ Molybdenite Formula: MoS2 Habit: Fine, flaky crystals Description: Distributed sporadically through the breccia and a few flakes in vugs. |
ⓘ Pyrite Formula: FeS2 |
ⓘ Quartz Formula: SiO2 Colour: Reddish-brown Description: Iron oxide stained boxwork of quartz septa. |
ⓘ 'Wolframite Group' |
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
ⓘ | Chalcocite | 2.BA.05 | Cu2S |
ⓘ | Chalcopyrite | 2.CB.10a | CuFeS2 |
ⓘ | Molybdenite | 2.EA.30 | MoS2 |
ⓘ | Pyrite | 2.EB.05a | FeS2 |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Quartz | 4.DA.05 | SiO2 |
ⓘ | 'Wolframite Group' | 4.DB.30 va | |
Group 7 - Sulphates, Chromates, Molybdates and Tungstates | |||
ⓘ | Antlerite | 7.BB.15 | Cu3(SO4)(OH)4 |
ⓘ | Chalcanthite | 7.CB.20 | CuSO4 · 5H2O |
Unclassified | |||
ⓘ | 'Limonite' | - |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Antlerite | Cu3(SO4)(OH)4 |
H | ⓘ Chalcanthite | CuSO4 · 5H2O |
O | Oxygen | |
O | ⓘ Antlerite | Cu3(SO4)(OH)4 |
O | ⓘ Chalcanthite | CuSO4 · 5H2O |
O | ⓘ Quartz | SiO2 |
Si | Silicon | |
Si | ⓘ Quartz | SiO2 |
S | Sulfur | |
S | ⓘ Antlerite | Cu3(SO4)(OH)4 |
S | ⓘ Chalcopyrite | CuFeS2 |
S | ⓘ Chalcanthite | CuSO4 · 5H2O |
S | ⓘ Chalcocite | Cu2S |
S | ⓘ Molybdenite | MoS2 |
S | ⓘ Pyrite | FeS2 |
Fe | Iron | |
Fe | ⓘ Chalcopyrite | CuFeS2 |
Fe | ⓘ Pyrite | FeS2 |
Cu | Copper | |
Cu | ⓘ Antlerite | Cu3(SO4)(OH)4 |
Cu | ⓘ Chalcopyrite | CuFeS2 |
Cu | ⓘ Chalcanthite | CuSO4 · 5H2O |
Cu | ⓘ Chalcocite | Cu2S |
Mo | Molybdenum | |
Mo | ⓘ Molybdenite | MoS2 |
Other Regions, Features and Areas containing this locality
North America PlateTectonic Plate
- Basin and Range BasinsBasin
- Mojave DomainDomain
This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to
visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders
for access and that you are aware of all safety precautions necessary.