Swede Mine

The Swede Mine is a tungsten mine located in Pinal county, Arizona at an elevation of 4,350 feet.

About the MRDS Data:

All mine locations were obtained from the USGS Mineral Resources Data System. The locations and other information in this database have not been verified for accuracy. It should be assumed that all mines are on private property.

Mine Info

Name: Swede Mine  

State:  Arizona

County:  Pinal

Elevation: 4,350 Feet (1,326 Meters)

Commodity: Tungsten

Lat, Long: 33.36111, -110.99167

Map: View on Google Maps

Satelite View

MRDS mine locations are often very general, and in some cases are incorrect. Some mine remains have been covered or removed by modern industrial activity or by development of things like housing. The satellite view offers a quick glimpse as to whether the MRDS location corresponds to visible mine remains.


Satelite image of the Swede Mine

Swede Mine MRDS details

Site Name

Primary: Swede Mine
Secondary: Swede Mine and Clark Prospect
Secondary: Cole Tungsten Prospect
Secondary: Old Swede Mine


Commodity

Primary: Tungsten
Tertiary: Copper
Tertiary: Lead
Tertiary: Zinc
Tertiary: Molybdenum


Location

State: Arizona
County: Pinal
District: Summit District


Land Status

Land ownership: National Forest
Note: the land ownership field only identifies whether the area the mine is in is generally on public lands like Forest Service or BLM land, or if it is in an area that is generally private property. It does not definitively identify property status, nor does it indicate claim status or whether an area is open to prospecting. Always respect private property.


Holdings

Not available


Workings

Type: Surface/Underground


Ownership

Owner Name: Helen Marie Cole


Production

Year: 1942
Description: Ap_Grade: ^Yielded 60 Lbs Of Conc Assaying 32.4% W03


Deposit

Record Type: Site
Operation Category: Past Producer
Operation Type: Unknown
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

General Physiographic Area: Intermontane Plateaus
Physiographic Province: Basin And Range Province
Physiographic Section: Mexican Highland


Mineral Deposit Model

Not available


Orebody

Not available


Structure

Type: L
Description: Ne Shear Zone, Fault Displacing Vein 20 Ft


Alterations

Not available


Rocks

Name: Granite
Role: Associated
Age Type: Host Rock
Age Young: Paleocene

Name: Granite
Role: Associated
Age Type: Host Rock Unit
Age Young: Neoproterozoic

Name: Granite
Role: Associated
Age Type: Associated Rock
Age Young: Pliocene

Name: Granite
Role: Associated
Age Type: Associated Rock Unit
Age Young: Paleocene


Analytical Data

Not available


Materials

Ore: Chalcopyrite
Ore: Galena
Ore: Pyrite
Ore: Scheelite
Ore: Wolframite
Ore: Sphalerite
Ore: Molybdenite
Gangue: Limonite
Gangue: Hematite
Gangue: Quartz
Gangue: Jarosite


Comments

Comment (Deposit): MOST OF WOLFRAMITE S OF FAULT CONFINED TO 10 INCH STREAK ON HANGING WALL AT SURFACE AND ON FOOTWALL IN CROSSCUT

Comment (Geology): SWEDE VEIN TRAVERSES AN IRREGULAR TONGUE OF PINAL SCHIST PROJECTING INTO GRANITE ALONG A SHEAR ZONE SLIGHTLY DISCORDANT WITH SCHISTOSITY . REPLACEMENT MOST COMPLETE WHERE SHEAR ZONE IS INTERSECTED BY GRANITE PORPHYRY DIKES.

Comment (Deposit): THIS REPORT REPRESENTS A MERGER OF ORIGINAL RECORD M000667 WITH RECORD M030484 OF JAN WILT IN MOLYBDENUM FILE, CONTACT PERSON T.G. THEODORE, USGS ; INFO.SRC : 1 PUB LIT; 2 UNPUB REPT

Comment (Location): INFO FROM LAND.ST :1979

Comment (Development): 2 UNPATENTED LODE CLAIMS

Comment (Workings): ADIT CROSSCUT AND DRIFTS. SMALL OPEN CUTS, PITS, AND PROSPECT HOLES


References

Reference (Deposit): PETERSON, 1963, USGS BULL 1141-H

Reference (Deposit): DALE, 1959, USBM RI 5516

Reference (Deposit): ABM FILE DATA

Reference (Production): PETERSON, 1963


Arizona Gold

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"Where to Find Gold in Arizona" looks at the density of modern placer mining claims along with historical gold mining locations and mining district descriptions to determine areas of high gold discovery potential in Arizona. Read more: Where to Find Gold in Arizona.