Manning Creek Deposit

The Manning Creek Deposit is a aluminum, potassium, and kaolin mine located in Piute county, Utah at an elevation of 8,199 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: Manning Creek Deposit  

State:  Utah

County:  Piute

Elevation: 8,199 Feet (2,499 Meters)

Commodity: Aluminum, Potassium, Kaolin

Lat, Long: 38.42639, -112.09611

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 Manning Creek Deposit

Manning Creek Deposit MRDS details

Site Name

Primary: Manning Creek Deposit


Commodity

Primary: Aluminum
Primary: Potassium
Primary: Kaolin


Location

State: Utah
County: Piute
District: Marysvale Region


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

Not available


Ownership

Not available


Production

Not available


Deposit

Record Type: Site
Operation Category: Occurrence
Deposit Type: Replacement
Operation Type: Unknown
Discovery Year: 1915
Discovery Method: Ore-Mineral In Place
Years of Production:
Organization:
Significant: N
Deposit Size: M


Physiography

General Physiographic Area: Intermontane Plateaus
Physiographic Province: Colorado Plateaus
Physiographic Section: High Plateaus Of Utah
Physiographic Detail: Straight Canyon


Mineral Deposit Model

Not available


Orebody

Form: IRREGULAR


Structure

Not available


Alterations

Not available


Rocks

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

Name: Latite
Role: Associated
Age Type: Host Rock Unit
Age Young: Oligocene

Name: Latite
Role: Associated
Age Type: Host Rock
Age Young: Pliocene


Analytical Data

Analytical Data: CHEMICAL ANALYSIS SHOWS 5 SAMPLES RANGE FROM 0 % TO 47 % ALUNITE


Materials

Ore: Alunite
Ore: Kaolinite


Comments

Comment (Workings): CALLAGHAN ( 1973 , P. 115 ) REPORTS A SHORT ADIT, LONG ADIT, AND A SHAFT

Comment (Reserve-Resource): CALLAGHAN ( 1973 ) COMMENTS THAT MUCH PHYSICAL EXPLORATION IS REQUIRED TO DETERMINE IF AN ECONOMICALLY VIABLE OPERATION COULD BE UNDERTAKEN

Comment (Reserve-Resource): QUOTE OF AN UNPUB EST BY M. E. WILLARD

Comment (Location): SLOPES EITHER SIDE OF STRAIGHT CREEK, A SOUTH BRANCH OF MANNING CREEK ABOUT A MILE EAST OF THE CANYON MOUTH

Comment (Commodity): PROJECT 9350 - 01393 ALUNITE RESOURCES

Comment (Geology): WILLARD REPORTS CONSIDERABLE PYRITE APPEARING IN THE SOUTH ADIT

Comment (Deposit): Discovery Year: WW1


References

Reference (Analytical Data): SRC.REF: CALLAGHAN, E., 1973 , UTAH GEOL. AND MINERALOG. SURVEY BULL. 102 , P. 117

Reference (Deposit): CALLAGHAN, E., 1973 , MINERAL RESOURCE POTENTIAL OF PIUTE COUNTY, UTAH AND ADJOINING AREA: UTAH GEOL. AND MINERALOG. SURVEY BULL. 102 , P. 115 - 117

Reference (Deposit): CALLAGHAN, E.,1938, PRELIMINARY REPORT ON THE ALUNITE DEPOSITS OF THE MARYSVALE REGION, UTAH: U.S. GEOLOGICAL SURVEY BULLETIN 886D, P.91-134.

Reference (Deposit): THOENEN, J.R.,1941, ALUNITE RESOURCES OF THE UNITED STATES, U.S. BUREAU OF MINES REPORT OF INVESTIGATION 3561, 48 P.

Reference (Deposit): 1918 DIREXPL UNKNOWN: SHAFT, ADITS

Reference (Deposit): 1938 RECON E. CALLAGHAN: BULL. 886-D

Reference (Deposit): 1943 GEOLMAP M. E. WILLARD: UTAH GEOL. AND MINERALOG. SURVEY BULL. 102 , FIG. 70


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