Sunday Tunnel

The Sunday Tunnel is a lead and silver mine located in Utah county, Utah at an elevation of 9,701 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: Sunday Tunnel  

State:  Utah

County:  Utah

Elevation: 9,701 Feet (2,957 Meters)

Commodity: Lead, Silver

Lat, Long: 40.54972, -111.62361

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 Sunday Tunnel

Sunday Tunnel MRDS details

Site Name

Primary: Sunday Tunnel


Commodity

Primary: Lead
Primary: Silver


Location

State: Utah
County: Utah
District: American Fork 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

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Past Producer
Deposit Type: Vein
Operation Type: Unknown
Year Last Production: 1880
Discovery Year: 1875
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: S


Physiography

General Physiographic Area: Rocky Mountain System
Physiographic Province: Middle Rocky Mountains
Physiographic Detail: Wasatch Mountains


Mineral Deposit Model

Not available


Orebody

Form: TABULAR


Structure

Type: R
Description: Uinta-Cottonwood Arch, Cordilleran Hingeline, Sevier Overthrust Belt

Type: L
Description: Northeast Striking Fissure


Alterations

Alteration Type: L
Alteration Text: Oxidation


Rocks

Name: Quartzite
Role: Host
Age Type: Host Rock Unit
Age Young: Late Cambrian

Name: Quartzite
Role: Host
Age Type: Host Rock
Age Young: Late Cambrian


Analytical Data

Analytical Data: UNKNOWN


Materials

Ore: Galena
Ore: Argentite
Gangue: Quartz


Comments

Comment (Location): TOWNSHIP UNSURVEYED ; INFO FROM LAND.ST :1983

Comment (Production): SAID TO HAVE PRODUCED 17,000 DOLLARS WORTH OF ORE

Comment (Deposit): APPARENTLY A FISSURE DEPOSIT WITH LEAD-SILVER MINERALIZATION

Comment (Workings): WORKINGS CONSIST OF TWO ADITS AND ONE SHAFT. THE SUNDAY TUNNEL IS THE MAJOR WORKING AND HAS AN APPROXIMATE LENGTH OF 300 FT

Comment (Development): APPARENTLY ALL WORK DONE AT THIS MINE WAS PRIOR TO 1880

Comment (Deposit): Discovery Year: LATE 1800'S


References

Reference (Deposit): BUTLER, B.S., LOUGHLIN, G.F., HEIKES, V.C., AND OTHERS, 1920, THE ORE DEPOSITS OF UTAH: U.S. GEOLOGICAL SURVEY PROF. PAPER NO. 111.

Reference (Deposit): BAKER, A.A., CALKINS, F.C., CRITTENDEN, M.D., JR., AND BROMFIELD, C.S., 1966, GEOLOGIC MAP OF THE BRIGHTON QUADRANGLE, UTAH: U.S. GEOLOGICAL SURVEY GEOL. QUAD. MAP GQ-534

Reference (Production): BUTLER, 1920

Reference (Deposit): CALKINS, F.C., AND BUTLER, B.S., 1943, GEOLOGY AND ORE DEPOSITS OF THE COTTONWOOD-AMERICAN FORK AREA, UTAH: U.S. GEOLOGICAL SURVEY PROF. PAPER NO. 201.


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