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Magmatic Copper Mine (Magmatic Copper Company claims; Stacy claims; Lode Star claims), Apache Leap, Superior, Pinal County, Arizona, USAi
Regional Level Types
Magmatic Copper Mine (Magmatic Copper Company claims; Stacy claims; Lode Star claims)Mine
Apache LeapCliff
SuperiorTown
Pinal CountyCounty
ArizonaState
USACountry

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Latitude & Longitude (WGS84):
33° 15' 20'' North , 111° 5' 21'' West
Latitude & Longitude (decimal):
Type:
Nearest Settlements:
PlacePopulationDistance
Superior2,943 (2017)4.3km
Top-of-the-World231 (2011)13.8km
Queen Valley788 (2011)19.2km
Gold Camp10,159 (2011)20.4km
Miami1,783 (2017)26.0km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Gila County Gem & Mineral SocietyMiami, Arizona26km
Apache Junction Rock and Gem ClubApache Junction, Arizona46km
Mindat Locality ID:
51590
Long-form identifier:
mindat:1:2:51590:3
GUID (UUID V4):
0


A group of 7 Mn-Au-Ag-Fe claims located in sec. 14, T2S, R12E, in the low-lying hills at the base of the westerly slope of Apache Leap (W of highway 177 [Superior-Ray Road]), about 2 miles South of Superior, at 3,000 feet of altitude. Owned by the Magmatic Copper Co. (1930). The claims extend into secs. 11 & 15.

Rocks exposed are quartzite, limestone, diabase and dacite. The quartzite forms the base of the series, and it is overlain by several hundred feet of massive limestone. A large mass of diabase is intruded into the limestone on the East sideof the claim group. South of the working shaft, between 2 faults, is an area of dacite identical with the rock forming the drest of Apache Leap. The sedimentary rocks strike about North and dip 35ºE. A prominant Northward-trending fault can be traced for several thousand feet on the claims. It cuts the limestone and South of the shaft, brings dacite into contact with the limestone.

Mineralization is manganese deposits that occur in the fault fissures or along bedding planes of Escabrosa Limestone adjacent to the faults. Lenses of manganous iron ore a few feet long occur along the faults, associated with silicified limestone and jasper. They dip 40W and are 3.05 meters thick.

Material from the working shaft is granular and dark brown and crumbles to a powder on exposure to air. Fresh pieces show specks and narrow seams of manganese oxides in the predominantly reddish-brown iron oxides. Many pieces show partly decomposed, coarse crystals of a brownish spar which may be manganous siderite.

Area structures include a minor N-S fault at the south end of the Concentrator Fault System; N-S-trending fault systems; N-S-trending sediments with a E dip; and various E-W-trending faults.

Workings include a 130 foot deep shaft and several older shafts at 50, 80 & 100 feet deep, respectively, and a 100 foot long tunnel.

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Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


4 valid minerals.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

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Alphabetical List Tree Diagram

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 4 - Oxides and Hydroxides
ⓘQuartz4.DA.05SiO2
ⓘPyrolusite4.DB.05Mn4+O2
Group 5 - Nitrates and Carbonates
ⓘCalcite5.AB.05CaCO3
ⓘSiderite5.AB.05FeCO3
Unclassified
ⓘ'Limonite'-
ⓘ'Wad'-

List of minerals for each chemical element

CCarbon
Cⓘ CalciteCaCO3
Cⓘ SideriteFeCO3
OOxygen
Oⓘ CalciteCaCO3
Oⓘ PyrolusiteMn4+O2
Oⓘ QuartzSiO2
Oⓘ SideriteFeCO3
SiSilicon
Siⓘ QuartzSiO2
CaCalcium
Caⓘ CalciteCaCO3
MnManganese
Mnⓘ PyrolusiteMn4+O2
FeIron
Feⓘ SideriteFeCO3

Other Databases

Link to USGS MRDS:10092689

Other Regions, Features and Areas containing this locality


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