Smith Mine

The Smith Mine is a iron mine located in Iron county, Utah at an elevation of 5,650 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: Smith Mine  

State:  Utah

County:  Iron

Elevation: 5,650 Feet (1,722 Meters)

Commodity: Iron

Lat, Long: 37.74083, -113.19722

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 Smith Mine

Smith Mine MRDS details

Site Name

Primary: Smith Mine


Commodity

Primary: Iron


Location

State: Utah
County: Iron
District: Iron Springs


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: Surface


Ownership

Owner Name: Utah International, Inc.


Production

Not available


Deposit

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


Physiography

Not available


Mineral Deposit Model

Not available


Orebody

Form: TABULAR


Structure

Type: R
Description: Sevier Thrust System

Type: L
Description: The Three Peaks Intrusion


Alterations

Alteration Type: L
Alteration Text: Limonitization


Rocks

Name: Quartz Monzonite
Role: Associated
Age Type: Host Rock Unit
Age Young: Late Jurassic

Name: Quartz Monzonite
Role: Associated
Age Type: Associated Rock Unit
Age Young: Pliocene

Name: Quartz Monzonite
Role: Associated
Age Type: Host Rock
Age Young: Late Jurassic

Name: Quartz Monzonite
Role: Associated
Age Type: Associated Rock
Age Young: Pliocene


Analytical Data

Analytical Data: IRON 64.5%


Materials

Ore: Hematite
Ore: Magnetite
Ore: Limonite
Gangue: Calcite
Gangue: Quartz
Gangue: Apatite


Comments

Comment (Deposit): METASOMATIC REPLACEMENT OF HOMESTAKE LIMESTONE WHICH OCCURS AS A ROOF PENDANT IN QUARTZ MONZONITE PORPHYRY. THE ORE IS ASSOCIATED WITH A RECUMBENT FOLD NORTH OF THE HOMESTAKE LIMESTONE, IS BOUNDED ON BOTH SIDES BY BASAL SILTSTONE MBR OF CARMEL

Comment (Location): SECTION SUBDIVISIONS SW 1/4 NW 1/4 SW 1/4

Comment (Workings): BENCH MINE WITH NUMEROUS LARGE PITS AND SHALLOW PROSPECT SURFACE PIT TO NE OF SMITH MINE


References

Reference (Deposit): 1947 RECON MACKIN, UTAH GEOL SOC GUIDEBOOK #2

Reference (Deposit): MACKIN, J HOOVER, 1947, SOME STRUCTURAL FEATURES OF THE INTRUSIONS IN THE IRON SPRINGS DISTRICT, UTAH: UTAH GEOL SOC GUIDEBOOK TO THE GEOLOGY OF UTAH, NO 2, 62 P

Reference (Deposit): MACKIN, J HOOVER, AND ROWLEY, PETER D, 1976, GEOL MAP OF THE CEDAR CITY NW QUADRANGLE, IRON COUNTY, UTAH: US GEOL SURVEY MAP GQ-1295

Reference (Deposit): BULLOCK, KENNETH C, 1973, GEOLOGY AND IRON DEPOSITS OF IRON SPRINGS DISTRICT, IRON COUNTY UTAH: BRIG YOUNG UNIV GEOLOGY STUDIES, VOL 20 PT 1, P 27-63.

Reference (Deposit): BULLOCK, KENNETH C, 1976, IRON DEPOSITS OF UTAH: UTAH GEOL AND MINERAL SURVEY BULLETIN 88, P 23-63.

Reference (Deposit): 1954 GEOLMAP MACKIN, MINERAL INVESTIGATIONS MAP MF-14

Reference (Deposit): 1967 RECON BLANK AND MACKIN, PROF PAPER 516-B

Reference (Deposit): 1973 RECON BULLOCK, BYU GEOL STUDIES V 20, PT 1

Reference (Deposit): 1976 GEOLMAP MACKIN AND ROWLEY, MAP GQ-1295

Reference (Deposit): 1976 RECON BULLOCK, UTAH GEOL AND MINERAL SURVEY BULLETIN 88

Reference (Production): BULLOCK, 1976, UGMS BULLETIN 88


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