Maple Shaft

The Maple Shaft is a mine located in Utah county, Utah at an elevation of 6,709 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: Maple Shaft  

State:  Utah

County:  Utah

Elevation: 6,709 Feet (2,045 Meters)

Commodity:

Lat, Long: 39.94611, -112.08833

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 Maple Shaft

Maple Shaft MRDS details

Site Name

Primary: Maple Shaft
Secondary: C.E. Loose Tract


Commodity

Tertiary: Lead
Tertiary: Silver


Location

State: Utah
County: Utah
District: Tintic District


Land Status

Land ownership: Private
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: Underground


Ownership

Owner Name: Clarence Loose
Home Office: Salt Lake City, Ut.


Production

Not available


Deposit

Record Type: Site
Operation Category: Occurrence
Operation Type: Unknown
Discovery Year: 1899
Discovery Method: Unknown
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

General Physiographic Area: Intermontane Plateaus
Physiographic Province: Basin And Range Province
Physiographic Section: Great Basin
Physiographic Detail: Thomas Mountains - Tintic Mountains


Mineral Deposit Model

Not available


Orebody

Form: IRREGULAR


Structure

Type: R
Description: N


Alterations

Alteration Type: L
Alteration Text: Argillization


Rocks

Name: Welded Tuff
Role: Associated
Age Type: Host Rock
Age Young: Late Ordovician

Name: Welded Tuff
Role: Associated
Age Type: Host Rock Unit
Age Young: Late Ordovician

Name: Welded Tuff
Role: Associated
Age Type: Associated Rock Unit
Age Young: Oligocene

Name: Welded Tuff
Role: Associated
Age Type: Associated Rock
Age Young: Oligocene


Analytical Data

Not available


Materials

Not available


Comments

Comment (Location): HIGH IN BURRISTON CANYON ; INFO FROM LAND.ST :1977

Comment (Deposit): NO ORE PRODUCED

Comment (Workings): SHAFT; PROBABLE DRIFT FROM YANKEE MINT AT 2000 LEVEL

Comment (Geology): EXPLORED BECAUSE OF PROXIMITY TO GOOD PRODUCERS


References

Reference (Deposit): MORRIS, H.T., 1964, GEOLOGY OF THE EUREKA QUADRANGLE, UTAH AND JUAB COUNTIES, UTAH: U.S. GEOLOGICAL SURVEY BULLETIN 1142-K, P. K1-K29.

Reference (Deposit): LINDGREN, WALDEMAR, AND LOUGHLIN, G.F., 1919, GEOLOGY AND ORE DEPOSITS OF THE TINTIC MINING DISTRICT, UTAH: U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 107, 276 PP.

Reference (Deposit): COOK, D.R., ED., 1957, GEOLOGY OF THE EAST TINTIC MOUNTAINS AND ORE DEPOSITS OF THE TINTIC MINING DISTRICTS: UTAH GEOL. SOC. GUIDEBOOK, NO. 12, 183 P.

Reference (Deposit): MORRIS, H.T., AND LOVERING, T.S., 1979, GENERAL GEOLOGY AND MINES OF THE EAST TINTIC MINING DISTRICT, UTAH AND JUAB COUNTIES, UTAH: U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1024, 194 PP.


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